NZ-AU: Sal de Vida Update Delivers Improved Economics, Resource and Reserve

• Nature and quality of sampling (eg cut channels, random chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc). These examples should not be taken as limiting the broad meaning of sampling.
• Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used.
• Aspects of the determination of mineralisation that are Material to the Public Report.
• In cases where ‘industry standard’ work has been done this would be relatively simple (eg ‘reverse circulation drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay’). In other cases more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (eg submarine nodules) may warrant disclosure of detailed information.

• Drainable porosity and brine sampling was conducted at accredited laboratories. Drill cuttings were described and stored in labelled plastic cutting boxes onsite. Sampled wells include diamond drillholes (for the analysis of drainable porosity and brine chemistry) as well as reverse circulation wells (to analyze brine chemistry). Core was described at 1-m intervals. Downhole geophysical logging was completed for the Phase 2 to Phase 5 programs, and consisted of gamma ray, resistivity, spontaneous-potential surveys, and borehole magnetic resonance and spectral gamma ray.
• Neither porosity (core) nor chemistry (brine) samples were subjected to any further preparation prior to shipment to participating laboratories. After the samples were sealed on site, they were stored in a cool location, and then shipped in sealed containers to the laboratories for analysis.
• Brine samples were handled by experienced geoscientists with a rigorous QA/QC program in place. An accredited laboratory was selected as the primary laboratory to assay the brine samples, and 5 secondary QA/QC labs were used throughout the drilling programs.
• -For drainable porosity sampling, Full diameter core with no visible fractures was selected and submitted for laboratory analyses. The selected sleeved core samples were capped with plastic caps, sealed with tape, weighed, and stored for shipment. The typical sample length was 15 – 40 cm.

-Brine samples were collected by drive-point samplers, centrifuge to confirm the drive-point sampling methodology, low-flow pumping and directly collected from the discharge line near the end of each pumping test for reverse circulation wells.

• Drill type (eg core, reverse circulation, open-hole hammer, rotary air blast, auger, Bangka, sonic, etc) and details (eg core diameter, triple or standard tube, depth of diamond tails, face-sampling bit or other type, whether core is oriented and if so, by what method, etc).

• -Throughout the 6 phases of drilling, a range of drill types and sizes were used. Each phase is broken out here.

-Phase 1: Core holes (6.4cm and 4.8cm) and conventional circulation mud-rotary drills were used (4.8cm).

-Phase 2: Core holes (6.4cm and 4.8cm) and conventional circulation mud-rotary drill were used (20.3cm).

-Phase 3: All wells were drilled by conventional mud rotary circulation. Drilled borehole diameters were 17.5 inches (444.5 mm), 12.25 inches (311.2 mm) and 8 inches (203.2 mm).

-Phase 4: rotary drill rig and completed with 10-inch PVC casing and gravel pack filter.

-Phase 5: rotary drill rig and completed with 8-inch PVC casing and gravel pack filter.

-Phase 6: The wells were drilled by conventional mud rotary circulation. Drilled borehole diameters were 24 inches (609.6 mm), 16 inches (406.4 mm) and 8.75 inches (222.25 mm). Once drilling was completed, production wells were cased with 10-inch (254 mm) blank PVC casing and a PVC well screen (slot size 0.75 mm). Gravel pack (1 – 2 mm and 1 – 3 mm diameters sand) was installed in the annular space surrounding the well screen. A bentonite seal was installed above the gravel pack, then cement and fill material were placed to the level of the land surface.

• Method of recording and assessing core and chip sample recoveries and results assessed.
• Measures taken to maximise sample recovery and ensure representative nature of the samples.
• Whether a relationship exists between sample recovery and grade and whether sample bias may have occurred due to preferential loss/gain of fine/coarse material.

• -Unwashed and washed drill cuttings from the exploration and RC wells were described and stored in labelled plastic cutting boxes. Core was described at 1-m intervals.

-Recovery percentages of drill core were recorded for each core hole; percent recovery was excellent for the majority of the samples obtained, except for weakly cemented, friable clastic sediments.

-The core holes descriptions are qualitative and quantitative. It allows the geoscientist to qualify the lithology, while quantitatively providing porosity measurements.

Cutting samples were not analysed chemically and descriptions were a qualitative evaluation of the lithologies encountered in the hole. There is no relationship between sample recovery and ion concentrations in the brine in this case.

• Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies.
• Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc) photography.
• The total length and percentage of the relevant intersections logged.

• Exploration to date has identified the Sal de Vida brine, and has used exploration methodology conventional to brine exploration, such as geophysics and surface sampling, in addition to the drilling programs. In the CP’s opinion, the drill data and hydrogeological studies are acceptable to support the Brine Mineral Resource and Ore Reserve estimates.
• -The core logging has been both qualitative and quantitative, and accomplished to a level appropriate for the resource estimation. Field logging is considered qualitative, where the lab analyses for drainable porosity is quantitative.

-Cuttings logging is of a qualitative nature and results were compared with the quantitative geophysical logs to interpret the lithologies encountered in the hole.

• All intersections with sample recovery were logged, and total drilled lengths and percent recovery recorded.

• If core, whether cut or sawn and whether quarter, half or all core taken.
• If non-core, whether riffled, tube sampled, rotary split, etc and whether sampled wet or dry.
• For all sample types, the nature, quality and appropriateness of the sample preparation technique.
• Quality control procedures adopted for all sub-sampling stages to maximise representivity of samples.
• Measures taken to ensure that the sampling is representative of the in situ material collected, including for instance results for field duplicate/second-half sampling.
• Whether sample sizes are appropriate to the grain size of the material being sampled.

• Brine samples were collected by drive-point samplers, micro samples were centrifuged from core to confirm the drive-point sampling methodology, low-flow pumping and directly collected from the discharge line near the end of each pumping test for reverse circulation wells.
• Neither porosity (core) nor chemistry (brine) samples were subjected to any further preparation prior to shipment to participating laboratories. After the samples were sealed on site, they were stored in a cool location, and then shipped in sealed containers to the laboratories for analysis.
• Analytical quality for the brine samples was monitored through the use of randomly inserted quality control samples, including standard reference materials (SRMs), blanks and duplicates, as well as check assays at independent laboratories. Each batch of samples submitted to the laboratory contained at least one blank, one low-grade SRM, one high-grade SRM and sample duplicates. Approximately 38% of the samples submitted for analysis were quality control samples.
• Duplicates, Standards and Blanks were used in the QA/QC program as well as up to 5 external laboratories to verify the data.
• Both brine and core samples were determined by the laboratories to be of adequate size for reliable analyses.

• The nature, quality and appropriateness of the assaying and laboratory procedures used and whether the technique is considered partial or total.
• For geophysical tools, spectrometers, handheld XRF instruments, etc, the parameters used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivation, etc.
• Nature of quality control procedures adopted (eg standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (i.e. lack of bias) and precision have been established.

-The brine chemistry tests are based upon American Public Health Association (APHA), Standard Methods for Examination of Water and Wastewater, Environmental Protection Agency (EPA), and American Society for Testing Materials (ASTM) protocols.

-Physical parameters, such as pH, conductivity, density, and TDS are directly determined from the brine samples. Analysis of lithium, potassium, calcium, sodium and magnesium is achieved by fixed dilution of filtered samples and direct aspiration into atomic absorption (AA) or inductively coupled plasma (ICP) instruments. All methods are considered to be industry standard methods.

• All tools used were in accordance with the ISO 9001 accreditation and consistent with ISO 17025 methods at other laboratories. All laboratories used to analyse samples for the Resource Estimate were/are independent of Allkem.
• -Analytical quality was monitored through the use of randomly inserted quality control samples, including standard reference materials (SRMs), blanks and duplicates, as well as check assays at independent laboratories. Each batch of samples submitted to the laboratory contained at least one blank, one low-grade SRM, one high-grade SRM and two sample duplicates. Approximately 38% of the samples submitted for analysis were quality control samples.

-The relative standard deviation values for the Standard Reference Materials ranged from 3.7 to 7.5, indicating good overall analytical reproducibility for the standard analyses conducted.

-The relative standard deviation values for the blanks range from 3.0 to 7.4, indicating good overall analytical reproducibility for standard analyses conducted at Alex Stewart.

-Sample and laboratory duplicate analyses indicated acceptable precision for lithium, potassium, and magnesium analyses conducted at Alex Stewart.

-The round robin analytical program conducted by the previous owner Lithium One at the beginning of the 2010 – 2011 drill program indicated comparable accuracy and precision to that achieved by Alex Stewart. For this reason, the University of Antofagasta was chosen as the check analysis laboratory for the 2010 drill program. Due to turnaround time delays using the University of Antofagasta, ACME was used as the check analysis laboratory for the 2011 drill program.

• The verification of significant intersections by either independent or alternative company personnel.
• The use of twinned holes.
• Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols.
• Discuss any adjustment to assay data.

• Verification by the CP Montgomery & Associates Consultores Limitada covered field exploration and drilling and testing activities. These included descriptions of drill core and cuttings, laboratory results for drainable porosity and chemical analyses, including quality control results, and review of surface and borehole geophysical surveys.
• No holes were twinned, duplicate brine samples were presented to the laboratories.
• -In the early phases of the Project, all data were transferred into a central data repository managed by Montgomery & Associates and other consultants. The database was originally located In Denver, Colorado and later synchronised with a data repository in the Project offices in Argentina, and a separate data repository at Montgomery and Associates’ offices In Tucson, Arizona. Currently, Allkem manages the main database.

-Raw data from the Project were transferred into a customised Access database and used to generate reports as needed.

-Field data were transferred by Field personnel into customised data entry templates. Field data were verified before being uploaded into the Access database using the methodology of crosschecking data between Field data sheets and Excel tables loaded in the server. data contained in the templates were loaded using an import tool, which eliminated data reformatting. Data were reviewed after database entry.

-Laboratory assay certificates were directly loaded into the Access database. Quality control reports were automatically generated for every imported assay certificate and reviewed by to ensure compliance with acceptable Quality control standards. Failures were reported to the Laboratory for correction.

-The drainable porosity and chemistry data used to support the Brine Resource estimates were verified. These verifications confirmed that the analytical results delivered by the participating laboratories and the digital exploration data were sufficiently reliable for Brine Resource estimation purposes. No adjustments to assay data are recorded.

• No adjustments to assay data are recorded.

• Accuracy and quality of surveys used to locate drill holes (collar and down-hole surveys), trenches, mine workings and other locations used in Mineral Resource estimation.
• Specification of the grid system used.
• Quality and adequacy of topographic control.

• All drill hole collar were surveyed using Trimble differential GPS instruments, handheld GPS or differential GNSS instrument. The North and East coordinates, elevation above ground level, elevation at the wellhead and stick-up elevation were provided through the RTK method and were linked to the official reference system and reference frame.
• Coordinates on UTM system (Universal Transverse Mercator), Datum GAUSS KRÛGGER-POSGAR 07

• Data spacing for reporting of Exploration Results.
• Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied.
• Whether sample compositing has been applied.

• -Exploration holes in general are spaced on a <1000m spacing in several locations over the site.</li>
• Exploration to date has identified the Sal de Vida brine, and has used exploration methodology conventional to brine exploration, such as geophysics and surface sampling, in addition to the drilling programs. In the CP’s opinion, the drill data and hydrogeological studies are acceptable to support the Brine Mineral Resource and Ore Reserve estimates.
• The samples taken during the pumping tests are composite samples, sourced from a single well, but pumped from multiple aquifer zones within that one well.

• Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type.
• If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to have introduced a sampling bias, this should be assessed and reported if material.

• The salar deposits that host lithium-bearing brines consist of sub-horizontal beds and lenses of sand, silt, halite, clay and minor gravels, depending on the location within the salar. Drill holes are vertical and essentially perpendicular to these units intersecting close to their true thickness.

• The measures taken to ensure sample security.

• All samples were labelled with permanent marker, sealed with tape and stored at a secure site until transported to the laboratory for analysis. Labels were hand-written in accordance with the chain-of-custody field data sheets. Samples were packed into secured boxes with chain-of- custody forms and shipped to the relevant laboratory.

• The results of any audits or reviews of sampling techniques and data.

• Geochemical Applications International has conducted laboratory audits of Alex Stewart as part of a round robin analysis for the 2010-2011 drill program.

• Type, reference name/number, location and ownership including agreements or material issues with third parties such as joint ventures, partnerships, overriding royalties, native title interests, historical sites, wilderness or national park and environmental settings.
• The security of the tenure held at the time of reporting along with any known impediments to obtaining a licence to operate in the area.

• – Sal de Vida (latitude 25° 24’ 33.71” South, longitude 66° 54’ 44.73” West) is located approximately 200 kilometres south of the Olaroz Project, Allkem’s operating mine in the high-altitude Puna ecoregion of the Altiplano of northwest Argentina at approximately 4,000 meters above sea level. Sal de Vida is within Salar del Hombre Muerto in the Province of Catamarca.

-Allkem’s mining tenement interests in the Sal de Vida Project are held by Galaxy Lithium (Sal de Vida) S.A., a wholly owned subsidiary of Galaxy Resources Ltd. (Australia) which in turn is 100% owned by Allkem Ltd since August 2021.

-Allkem currently has mineral rights over 26,253 ha at Salar del Hombre Muerto, which are held under 31 mining concessions. Allkem has been granted easements related to water, camps, infrastructure and services enabling commencement of Stage 1 construction. The Project is not subject to any known environmental liabilities other than those actions and remedies indicated in the Environmental Impact Study approval process.

-All the mining concessions for the Sal de Vida Project were secured under purchasing agreements with pre-existing owners and claimants. In some cases, sellers retained usufruct rights (a legal right accorded to a person or party that confers the temporary right to use and derive income or benefit from someone else’s mining property) and commercial rights (third-party rights) for the development of ulexite (borates) at surface.

-Pursuant to Argentinian Law 4757 (as amended), Catamarca Mining royalty is limited to 3% of the mine head value of the extracted ore, which consist in the sales price less direct cash costs related to exploitation (excluding fixed asset depreciation, the “Mining Royalty”).

-On December 20, 2021, GLSSA and the Governor of the Province of Catamarca subscribed a Royalties Commitment Deed (the “Royalty Agreement”), pursuant to which GLSSA agrees to pay to the Province of Catamarca a maximum amount of 3.5% of the “net monthly revenue” from the Project, as follows:

-The “Mining Royalty” will be paid as indicated by the provincial Royalty Regime.

-An “Additional Contribution” of 3.2% less the Mining Royalty and the applicable water canon; and

-0.3% shall be paid as a “Corporate Social Responsibility (CSR) Contribution”.

-The validity of the Royalty Agreement is subject to the approval of the Legislature of the Province of Catamarca, which is in due course to be obtained.

-The payment of Mining Royalty is due once the commercial production of the Sal de Vida Project commences and the payment of the Additional Contribution and CSR Contribution is due once the Province of Catamarca (through the relevant authority) grants GLSSA the relevant water concession pursuant to Section 7 of the Water Law No. 2577, as amended.

-The Additional Contribution and CSR Contribution will be paid through a Trust, pursuant to provincial legislation to be enacted.

-The 3.5% maximum amount shall be the maximum amount payable by GLSSA to the province of Catamarca, for any reason whatsoever, for the whole life of the Project (including any expansions).

-The “net monthly revenue” will be calculated by reference to the amounts invoiced by GLSSA each month for the sale of lithium products produced from the Project, and for the Mining Royalty, less (i) any taxes, duties, levies included on those invoiced amounts and (ii) any sales reimbursement.

• -Legal opinion provided supports that Allkem currently holds an indirect 100% interest in the Sal de Vida Project through its subsidiary Galaxy Lithium (Sal de Vida) S.A.

-Legal opinion provided supports that the mineral tenures held are valid and sufficient to support declaration of Brine Mineral Resources and Brine Ore Reserves.

-Social and permitting applications have sufficiently progressed to permit the commencement of Stage 1 construction. The CP is not aware of any significant environmental, social, or permitting issues that would prevent future exploitation of the Sal de Vida Project, other than as discussed in this Report.

• Acknowledgment and appraisal of exploration by other parties.

• No exploration by other parties is known for lithium carbonate.
• Prior mining was done on site for ulexite, within 5m of surface.

• Deposit type, geological setting and style of mineralisation.

• -The regional geological setting is the Altiplano Puna plateau, an area of uplift that began during the middle to late Miocene (10 – 15 Ma). Red-bed sediments formed during the early to middle Miocene in areas of structural depressions. During the middle to late Miocene, a combination of thrust faulting, uplift and volcanism led to the sedimentary basins becoming isolated. The Cordilleras and major watersheds bound the Puna area to the west and east. Sedimentation in these basins began with the formation of alluvial fans at the feet of the uplifted ranges and continued with the development of playa sandflats and mudflat facies.

-In basin areas, the watersheds are within the basins; there are no outlets from the basins. Ongoing runoff, both surface and underground, continued solute dissolution from the basins and concentration in their centres where evaporation is the only outlet. Evaporite minerals occur both as disseminations within a clastic sequence and as discrete beds.

-The Salar system in the Hombre Muerto basin is considered a typical mature salar. The Hombre Muerto basin has an evaporite core that is dominated by halite. Basin margins are steep and are interpreted to be fault controlled. The east basin margin is predominantly Pre-Cambrian metamorphic and crystalline rocks belonging to Pachamama formation. Volcanic tuff and reworked tuffaceous sediments, most likely from Cerro Galan complex, together with tilted Tertiary rocks, are common along the western and northern basin margins. In the Sal de Vida Project area, the dip angle of Tertiary sandstone is commonly about 45º to the southeast. Porous travertine and associated calcareous sediments are common in the subsurface throughout the basin and are flat lying; these sediments appear to form a marker unit that is encountered in most core holes at similar altitudes. Several exploration boreholes located near basin margins completely penetrated the flat-lying basin-fill deposits, and have bottoms in tilted Tertiary sandstone, volcanic tuff, and micaceous schist.

• A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drill holes:
  • easting and northing of the drill hole collar
  • elevation or RL (Reduced Level – elevation above sea level in metres) of the drill hole collar
  • dip and azimuth of the hole
  • down hole length and interception depth
  • hole length.
• If the exclusion of this information is justified on the basis that the information is not Material and this exclusion does not detract from the understanding of the report, the Competent Person should clearly explain why this is the case.

Notes: a = Coordinates on UTM system (Universal Transverse Mercator), Datum GAUSS KRÛGGER-POSGAR 07.

b = metres, amsl = above mean sea level

c = metres, bls = below land surface

All drill holes are vertical (dip -90, azimuth 0 degrees)

d = the table presents recent wells from Allkem (Lithium One exploration wells are not included)

• In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (eg cutting of high grades) and cut-off grades are usually Material and should be stated.
• Where aggregate intercepts incorporate short lengths of high grade results and longer lengths of low grade results, the procedure used for such aggregation should be stated and some typical examples of such aggregations should be shown in detail.
• The assumptions used for any reporting of metal equivalent values should be clearly stated.

• The pumping well samples are composite samples that reflect inflows from different levels within the wells, which are screened at multiple levels throughout their depth. The lithium concentration in the pumped samples is an average of the concentration from different units with relatively higher and lower values than the average. More permeable units contribute a higher proportion of the brine in the pumped samples.
• No other aggregate methods were used.
• Lithium carbonate equivalent (LCE) values are reported but are directly proportional to the amount of lithium in the resource brine. Therefore, they are not considered to be “equivalent” values as commonly defined in mining.

• These relationships are particularly important in the reporting of Exploration Results.
• If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported.
• If it is not known and only the down hole lengths are reported, there should be a clear statement to this effect (eg ‘down hole length, true width not known’).

• The sediments hosting brine are interpreted to be essentially perpendicular to the vertical drill holes, representing true thicknesses in drilling. Except in those areas where fresh water occurs in the upper part of the aquifer, the entire thickness of sediments is believed to be mineralized with lithium brine, with the water table within approximately 1 metre of surface in most part of the salar. Lithium is hosted in brine in pores within the different terrestrial sedimentary units in the salt lake sequence.

• Appropriate maps and sections (with scales) and tabulations of intercepts should be included for any significant discovery being reported These should include, but not be limited to a plan view of drill hole collar locations and appropriate sectional views.

Hydrogeological Cross-Section Locations (Plan View): 
https://www.globenewswire.com/NewsRoom/AttachmentNg/9e44d413-c250-4b5c-8131-5ee17e9de189

Hydrogeological Cross-Section A-A’: 
https://www.globenewswire.com/NewsRoom/AttachmentNg/4bf147ad-2352-436a-bf1c-c31260fd2b00

Hydrogeological Cross-Section B-B’:
https://www.globenewswire.com/NewsRoom/AttachmentNg/6ee3718a-a4b6-481d-a1d2-d8c4d57d6537

Hydrogeological Cross-Section C-C’:
https://www.globenewswire.com/NewsRoom/AttachmentNg/6ebc1ebf-d84a-4f51-9a02-59c578308c95

Hydrogeological Cross-Section D-D’:
https://www.globenewswire.com/NewsRoom/AttachmentNg/29ad6408-5e63-4141-954a-7c26a3084960

• Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high grades and/or widths should be practiced to avoid misleading reporting of Exploration Results.

• Exploration results are presented from all areas of the Sal de Vida mine concessions and are believed to representative. Reported results have not been screened, disregarded, or specifically selected to mislead the reader.

• Other exploration data, if meaningful and material, should be reported including (but not limited to): geological observations; geophysical survey results; geochemical survey results; bulk samples – size and method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock characteristics; potential deleterious or contaminating substances.

• -A number of geophysical surveys have been completed and are summarized in the Geophysical Survey table below. The gravity survey locations are shown in Location of Year 2021 Gravity Survey Lines, the vertical electric sounding point locations in Location Map, Vertical Electric Sounding Points, transient electromagnetic survey profile line locations in Location Map, Transient Electromagnetic Survey Profiles, and 2D and 3D reinterpretation of depth to basement rock at Sal de Vida Project is shown in 2D Plan View of Sal de Vida Basement Map and 3D Model Update of the Cerro Ratones Northeast Edge, respectively.
• Geophysical Surveys:
  https://www.globenewswire.com/NewsRoom/AttachmentNg/951fdcc4-c5b5-4894-9082-b408f397fae8

Location of Year 2021 Gravity Survey Lines:
https://www.globenewswire.com/NewsRoom/AttachmentNg/f6283ea9-d56b-43fc-83e3-54d366cf9c87
 
Location Map, Vertical Electric Sounding Points (Note: Figure from GEC Geophysical Exploration & Consulting S.A., 2010. Green represents VES readings and red proposed drill holes. Red triangles represent core holes):
https://www.globenewswire.com/NewsRoom/AttachmentNg/8817bbc1-492e-4410-b6ac-15fb985907de

Location Map, Transient Electromagnetic Survey Profiles:
https://www.globenewswire.com/NewsRoom/AttachmentNg/6c03d0c4-cc46-488f-90d9-5432503c98f3

2D Plan View of Sal de Vida Basement Map (Note: Tertiary Basement is indicated in green and in the Precambrian Basement is indicated in brownish yellow):
https://www.globenewswire.com/NewsRoom/AttachmentNg/34dee8dd-cf4e-495a-ac7e-c4fe85d5d82f

3D Model Update of the Cerro Ratones Northeastern Outcrop (Note: Tertiary Basement is indicated in green and the Precambrian Basement in gray with a 1:3 vertical exaggeration):
https://www.globenewswire.com/NewsRoom/AttachmentNg/9568a937-3c03-4cfd-a6e3-e8eb14723e96

-During the exploration program, downhole electrical conductivity surveys were conducted at many of the wells after completion and boreholes to identify fresh water and brine-bearing parts of the aquifer. Electrical conductivity is a measure of the water’s ability to conduct electricity and is an indirect measure of the water’s ionic activity and dissolved solids content. Electrical conductivity is positively correlated with brine concentration. The purpose of the profiles was to:

-Determine the electrical conductivity profile and identify potential freshwater influence and low density, and

-Provide additional verification for the chemistry profiles generated from depth-specific samples.

-Short-term pumping tests under operating conditions have demonstrated excellent brine extraction and aquifer recharge rates to support the production design basis.

-Long-term pumping tests under operating conditions at each wellfield did not show any significant or obvious change in the aquifer water chemistry entering the wellfields during the pumping period.

• The nature and scale of planned further work (eg tests for lateral extensions or depth extensions or large-scale step-out drilling).
• Diagrams clearly highlighting the areas of possible extensions, including the main geological interpretations and future drilling areas, provided this information is not commercially sensitive.

• -Exploration should be conducted to better identify and potentially demonstrate additional extractable brine in other parts of the basin. Favourable exploration results represent Project upside potential. The following additional investigations are recommended:

-Geophysical surveys: perform additional gravity, magnetic, and resistivity surveys over the east, south and west sub-basins to supplement the existing surveys.

-Core drilling: additional wells in the southwest and eastern portions of the mine concessions that are deeper than 300 m.

-Downhole sampling of any additional wells to obtain brine chemistry and drainable porosity results.

-Additional 30-day pumping tests to identify potential for new wellfields.

-Quality assurance and quality control (QA/QC) measures should be continued for all collected brine samples including the use of blanks, duplicates, standards, and secondary (external) laboratories to increase confidence in the obtained data. 10% to 20% of the collected samples should be analysed for QA/QC purposes, and a round-robin analysis of brine samples is recommended. The determination of drainable porosity should be confirmed with two independent methodologies including the analysis of core samples and indirect measurements (e.g., borehole magnetic resonance), among others.

• Measures taken to ensure that data has not been corrupted by, for example, transcription or keying errors, between its initial collection and its use for Mineral Resource estimation purposes.
• Data validation procedures used.

• Verification and validation of the assay data was performed for the 51 sample sites. Verification includes pH, density, conductivity, TDS, sulphate, Cl, alkalinity, B, Ca, K, Li, Mg and Na. Verification of the location of trenches and samples collected by use of differential GPS was also conducted.
• For the Feasibility Study, Montgomery and Associates personnel verified the drainable porosity and chemistry data used for the Brine Mineral Resource estimates. These verifications support that the analytical results delivered by the participating laboratories and the digital exploration data were sufficiently reliable for the Brine Mineral Resource and Brine Ore Reserve estimations outlined in this Report.

-A customized Access database was generated after integration between original database and raw data from the project. It included a crosschecking methodology, assays certificates, quality control standards.

-Database lithium grades include QA/QC procedures where standards, duplicates, blanks and check analysis were used.

-The CPs concluded that the information was acceptable to support Brine Resource estimation.

• Comment on any site visits undertaken by the Competent Person and the outcome of those visits.
• If no site visits have been undertaken indicate why this is the case.

• Consulting firm Montgomery & Associates Consultores Limitada is assigned as Qualified Persons and have supervised the technical report and take responsibility for its contents.
• Consulting firm Montgomery & Associates Consultores Limitada is responsible for the Mineral Resources estimates and they have visited the site in numerous occasions, from 2010 to the present, and have reviewed the exploration activities. The last visit was conducted from July 31 to August 02, 2023, where the pumping wells and pilot ponds were also reviewed.

• Confidence in (or conversely, the uncertainty of ) the geological interpretation of the mineral deposit.
• Nature of the data used and of any assumptions made.
• The effect, if any, of alternative interpretations on Mineral Resource estimation.
• The use of geology in guiding and controlling Mineral Resource estimation.
• The factors affecting continuity both of grade and geology.

• There is a high level of confidence in the geological model for the Project. Six Hydrogeological units are defined based on five dominating lithologies where drainable porosity and brine chemistry analysis were performed. Sal de Vida’s brine chemistry has a high lithium grade, low levels of magnesium, calcium and boron impurities and readily upgrades to battery grade lithium carbonate.
• Interpretation is based on drill core and cuttings, drilling and test results, brine chemistry and porosity laboratory analysis, aquifer testing results, geophysical survey and other information available from the work carried out between 2009 to date. Porosity samples were collected during 2010, 2011, and 2012 from intact HQ and NQ-core. Full diameter core with no visible fractures was selected and submitted to Core Laboratory Petroleum Servicios, Texas.
• In addition to the depth-specific brine samples obtained by drive-points during coring, brine samples used to support the reliability of the depth-specific samples included analyses of brine centrifuged from core samples, brine obtained from low flow sampling of the exploration core holes and brine samples obtained near the end of the pumping tests in the exploration and production wells. Brine chemistry samples were sent to Alex Steward lab, duplicates samples were sent to University of Antofagasta lab and ACME Santiago lab was used for check analysis. Duplicate samples were sent to ALS Chemex lab, Argentina.
• In the CP’s opinion, and based on the brine system deposit model, knowledge of the geological setting of the Salar and associated hydrogeological systems, all drill data and hydrogeological studies are acceptable to support the Brine Mineral Resource and Ore Reserve estimates.

• The extent and variability of the Mineral Resource expressed as length (along strike or otherwise), plan width, and depth below surface to the upper and lower limits of the Mineral Resource.

• The deposit type is a brine aquifer within a salar basin. The extent of the active model resources covers an area of 146 km² for Measured and Indicated Mineral Resources plus an area of 14.9 km² for Inferred Mineral Resources, with a total of 160.9 km².

• The nature and appropriateness of the estimation technique(s) applied and key assumptions, including treatment of extreme grade values, domaining, interpolation parameters and maximum distance of extrapolation from data points. If a computer assisted estimation method was chosen include a description of computer software and parameters used.
• The availability of check estimates, previous estimates and/or mine production records and whether the Mineral Resource estimate takes appropriate account of such data.
• The assumptions made regarding recovery of by-products.
• Estimation of deleterious elements or other non-grade variables of economic significance (eg sulphur for acid mine drainage characterisation).
• In the case of block model interpolation, the block size in relation to the average sample spacing and the search employed.
• Any assumptions behind modelling of selective mining units.
• Any assumptions about correlation between variables.
• Description of how the geological interpretation was used to control the resource estimates.
• Discussion of basis for using or not using grade cutting or capping.
• The process of validation, the checking process used, the comparison of model data to drill hole data, and use of reconciliation data if available.

• The employed methodology for Mineral Resources is polygon based where every polygon contains at least 1 diamond drill exploration or exploration well. The boundaries between polygon blocks are generally equidistant from diamond drill holes. The depth of each polygon is based on the total depth of each borehole, and the subsurface lithological column was separated into hydrogeologic units which vary with depth based on the lithologic logs and other available field information.
• Each polygon is given a representative value for drainable porosity and average lithium content based on laboratory analyses of samples collected during exploration drilling.
• The Mineral Resource was estimated by summing the aquifer volume multiplied by drainable porosity and lithium grade for each interval of the individual polygons and resource category.
• No deleterious elements have been modelled as part of the brine feed.

• Whether the tonnages are estimated on a dry basis or with natural moisture, and the method of determination of the moisture content.

• Moisture content of the cores was measured (porosity and density measurements were made), but because brine is extracted by pumping, the sediment moisture is not a relevant parameter for the Resource Estimate.

• The basis of the adopted cut-off grade(s) or quality parameters applied.

• A cut-off grade of 300 mg/l was conservatively used based on a breakeven cut-off grade for a projected lithium carbonate equivalent (LCE) price of US$20,000 per tonne over the entirety of the Life of Mine (LOM), as well as a grade tonnage curve.

• Assumptions made regarding possible mining methods, minimum mining dimensions and internal (or, if applicable, external) mining dilution. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider potential mining methods, but the assumptions made regarding mining methods and parameters when estimating Mineral Resources may not always be rigorous. Where this is the case, this should be reported with an explanation of the basis of the mining assumptions made.

• The Mineral Resource has been quoted in terms of brine volume, concentration of lithium and their product lithium carbonate (LCE).
• No mining or recovery factors have been applied (although the use of the drainable porosity and exclusion of polygon intervals below the 300 mg/L lithium cut-off grade supports the reasonable prospects for eventual economic extraction with the proposed mining methodology). It should be noted that conversion of resources to reserves for brine deposits is lower than that for hard rock deposits.

-Dilution of brine concentrations may occur over time and typically there are lithium losses in both the ponds and processing plant in brine mining operations.

-The conceptual mining method is recovering brine from the salt lake via a network of wells, the established practice on existing lithium brine projects.

-Detailed hydrologic studies of the salar have been undertaken (catchment and groundwater modelling) to evaluate the extractable resources and potential extraction rates.

• The basis for assumptions or predictions regarding metallurgical amenability. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider potential metallurgical methods, but the assumptions regarding metallurgical treatment processes and parameters made when reporting Mineral Resources may not always be rigorous. Where this is the case, this should be reported with an explanation of the basis of the metallurgical assumptions made.

• Lithium carbonate and potassium chloride is projected to be produced on site via conventional brine processing techniques and evaporation ponds to concentrate the brine prior to processing as currently Allkem’s Olaroz operation does. Brine composition from Sal de Vida (SDV) could be processed using similar processing technology to that applied in the Olaroz production facility, which has been successfully applied to produce lithium carbonate in the Allkem (Previously Orocobre) facilities.

• Assumptions made regarding possible waste and process residue disposal options. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider the potential environmental impacts of the mining and processing operation. While at this stage the determination of potential environmental impacts, particularly for a greenfields project, may not always be well advanced, the status of early consideration of these potential environmental impacts should be reported. Where these aspects have not been considered this should be reported with an explanation of the environmental assumptions made.

• -Impacts of the lithium carbonate production operation at the SDV salar include surface disturbance from the creation of extraction/processing facilities and associated infrastructure, accumulation of various salt tailings impoundments and extraction from brine and freshwater aquifers regionally. Lime is used to increase precipitation of impurities like magnesium and calcium solids. Precipitated salts are collected in ponds and later returned to the salar.

-A small fraction of waste solids is generated in the lithium carbonate plant, that are mainly impurities removed from the brine. The main solids are a mixture of magnesium hydroxide and calcium carbonate. Waste disposals areas will surround the evaporation ponds to the north, east and southeast.
-Waste disposals areas will surround the evaporation ponds to the north, east and southeast. This facility will consist of halite, muriate, and co-disposal stockpiles surrounding the halite ponds and will cover a total area of approximately 300 ha for Stage 1 and 600 ha for Stage 2.
-The project has fulfilled the required environmental and social assessments to progress into construction of Stage 1. The project is permitted by the provincial mining authorities and has provincial and federal permits. The project reflects positive, social and socio-economic benefits for local communities. Expansion Stage 2 permitting application process is still to commence.

• Whether assumed or determined. If assumed, the basis for the assumptions. If determined, the method used, whether wet or dry, the frequency of the measurements, the nature, size and representativeness of the samples.
• The bulk density for bulk material must have been measured by methods that adequately account for void spaces (vugs, porosity, etc), moisture and differences between rock and alteration zones within the deposit.
• Discuss assumptions for bulk density estimates used in the evaluation process of the different materials.

• Density measurements were taken as part of the drill core assessment. This included determining dry density and particle density as well as field measurements of brine density. Note that no mining of sediments is to be carried out, as brine is to be extracted by pumping. Consequently, sediments are not mined but the lithium and potassium are extracted by pumping.
• No bulk density was applied to the estimates because resources are defined by volume, rather than by tonnage.
• The salt unit can contain fractures and possibly voids which host brine and add to the drainable porosity.

• The basis for the classification of the Mineral Resources into varying confidence categories.
• Whether appropriate account has been taken of all relevant factors (ie relative confidence in tonnage/grade estimations, reliability of input data, confidence in continuity of geology and metal values, quality, quantity and distribution of the data).
• Whether the result appropriately reflects the Competent Person’s view of the deposit.

• The Mineral Resource has been classified in Measured, Indicated and Inferred Mineral Resource categories based on the confidence in the estimation and specific information available. For Measured and Indicated Mineral Resources, the following factors are considered: Level of understanding and reliability of the basin stratigraphy and the local hydrogeologic characteristics of the aquifer system, density of drilling and testing in the salar and uniformity of the results within the area, and available pumping test and historical production information.
• The CP believes that the amount of exploration information and understanding of the deposit supports the Mineral Resource classification. The CP also believes that there is substantial upside potential for increasing both the Mineral Resource categories, and also by increasing the total Mineral Resource volume by drilling in unexplored areas, and by drilling deeper.

• The results of any audits or reviews of Mineral Resource estimates.

• A preliminary audit was conducted by SRK Consultants in 2022.

• Where appropriate a statement of the relative accuracy and confidence level in the Mineral Resource estimate using an approach or procedure deemed appropriate by the Competent Person. For example, the application of statistical or geostatistical procedures to quantify the relative accuracy of the Mineral Resource within stated confidence limits, or, if such an approach is not deemed appropriate, a qualitative discussion of the factors that could affect the relative accuracy and confidence of the estimate.
• The statement should specify whether it relates to global or local estimates, and, if local, state the relevant tonnages, which should be relevant to technical and economic evaluation. Documentation should include assumptions made and the procedures used.
• These statements of relative accuracy and confidence of the estimate should be compared with production data, where available.

• Main uncertainties of the Mineral Resource include the location of aquifer boundaries and shallower than anticipated bedrock near hard rock outcrops. Furthermore, uncertainties include the lateral continuity of key aquifer zones, presence of fresh and brackish water that have the potential to dilute the brine in the wellfield area and assumed uniformity of average aquifer parameters within specific aquifer units. Even though these uncertainties exist, the CP conservatively assigned resource categories in a manner aligned with industry practices for lithium brine projects.
• The level of understanding and reliability of the basin stratigraphy, level of understanding of the local hydrogeologic characteristics of the aquifer system, density of drilling and testing in the Salar and general uniformity of results within an area are the main factors that could support an upgrade of the Mineral Resource categories.
• It is recommended that a resource block model be created instead of the polygon method to estimate the Lithium Brine Mineral Resource.
• To the extent known by the CP, there are no known environmental, permitting, legal, title, taxation, socioeconomic, marketing, political or other relevant factors that could affect the Mineral Resource estimate which are not discussed.

• Description of the Mineral Resource estimate used as a basis for the conversion to an Ore Reserve.
• Clear statement as to whether the Mineral Resources are reported additional to, or inclusive of, the Ore Reserves.

• The Mineral Resource used as the basis for the Ore Reserve Estimate was based on the information in Section 3 of this Table 1.
• Mineral Resources are reported inclusive of Ore Reserves.

• Comment on any site visits undertaken by the Competent Person and the outcome of those visits.
• If no site visits have been undertaken indicate why this is the case.

• Consulting firm Montgomery & Associates Consultores Limitada is assigned as Qualified Persons and have supervised the technical report and take responsibility for its contents.
• Consulting firm Montgomery & Associates Consultores Limitada is responsible for the Ore Reserves Estimates and they have visited the site in numerous occasions, from 2010 to the present, where they have reviewed the exploration activities. The last visit was conducted from July 31 to August 02, 2023, where the pumping wells and pilot ponds were also reviewed.

• The type and level of study undertaken to enable Mineral Resources to be converted to Ore Reserves.
• The Code requires that a study to at least Pre-Feasibility Study level has been undertaken to convert Mineral Resources to Ore Reserves. Such studies will have been carried out and will have determined a mine plan that is technically achievable and economically viable, and that material Modifying Factors have been considered.

• The Sal de Vida Project in Stage 1 is based on a Feasibility Study. The Stage 2 considers an expansion of the Project, and it is under a current Pre-Feasibility Study.

• The basis of the cut-off grade(s) or quality parameters applied.

• A cut-off grade of 300 mg/L was conservatively applied based on a long-term estimated LCE price of US$20,000 per tonne. Results for Proved and Probable Ore Reserves indicate an average extracted grade of 757 mg/L throughout the life of the project, which far exceeds the 300 mg/L cut-off grade, demonstrating that production is economically viable.

• The method and assumptions used as reported in the Pre-Feasibility or Feasibility Study to convert the Mineral Resource to an Ore Reserve (i.e. either by application of appropriate factors by optimisation or by preliminary or detailed design).
• The choice, nature and appropriateness of the selected mining method(s) and other mining parameters including associated design issues such as pre-strip, access, etc.
• The assumptions made regarding geotechnical parameters (eg pit slopes, stope sizes, etc), grade control and pre-production drilling.
• The major assumptions made and Mineral Resource model used for pit and stope optimisation (if appropriate).
• The mining dilution factors used.
• The mining recovery factors used.
• Any minimum mining widths used.
• The manner in which Inferred Mineral Resources are utilised in mining studies and the sensitivity of the outcome to their inclusion.
• The infrastructure requirements of the selected mining methods.

• The life of mining is project to 40 years. Mining production for the years 1 and 2 is taken from Stage 1 in the East wellfield, and for the following years 3-40, production will incorporate Stage 2 from the SW, SE and N well areas. Currently, well depths are down to approximately 200m only and this can change when new deeper exploration wells are drilled. All production wells will be connected through pipelines to centrally positioned booster ponds. The East Wellfield (Stage 1) is designed with 8 operating wells plus one on standby.
• Projections for Ore Reserves indicates that average annual rate production of brine from the east is set in 315 L/s and 191 L/s from the southwest. The initial average grade is expected to be roughly 805 mg/L and 815 mg/L, respectively.
• Extraction using wells is the appropriate extraction choice in salt lakes, as the lithium is dissolved in brine (fluid) and mining of unconsolidated sediments is not contemplated.
• Geotechnical parameters for brine extraction are different to hard rock mining, thus detailed geotechnical studies are not required. Due to the fact that the mining of this type of deposit does not involve excavations or underground workings (as with hard rock deposits), it is not necessary to carry out detailed geotechnical studies of the soil and rock strength parameters.
• Pit slope is not relevant for brine mining.
• Dilution of brine during pumping is simulated within the numerical model for the conversion of Mineral Resources into Ore Reserves.
• There are no minimum mining widths, as brine mining is not a selective mining method.
• The Inferred Mineral Resources are not included in current mining studies but are considered a possible source of future brine extraction when their resource classification is upgraded.
• Brine mining requires the provision of electricity and pipelines to the sites of wells from which brine is extracted. The pipelines pump brine to centralised collection ponds, from where it is pumped to the evaporation pond network. The brine is subject to the addition of lime in the evaporation ponds. Pumps are required to move brine between ponds and pump brine into the plant, where lithium carbonate product is produced. Electricity generators for wellfields and boosters will be used during the pre-production (1 year) and then will be fed by a power line.

• The metallurgical process proposed and the appropriateness of that process to the style of mineralisation.
• Whether the metallurgical process is well-tested technology or novel in nature.
• The nature, amount and representativeness of metallurgical test work undertaken, the nature of the metallurgical domaining applied and the corresponding metallurgical recovery factors applied.
• Any assumptions or allowances made for deleterious elements.
• The existence of any bulk sample or pilot scale test work and the degree to which such samples are considered representative of the orebody as a whole.
• For minerals that are defined by a specification, has the Ore Reserve estimation been based on the appropriate mineralogy to meet the specifications?

• The metallurgical process utilised for the production of lithium carbonate is based on solar evaporation of brine, prior to reacting lithium with carbon dioxide in the plant to produce lithium carbonate. In this way, much of the energy required for the process is provided naturally by the sun. Lithium preferentially remains within the brine, and other elements precipitate from the brine in response to their increasing concentration and saturation in the brine. Lime is added to the ponds to facilitate the precipitation of magnesium from the brine. Although more recent direct extraction processing techniques are more widely available pond evaporation provides a cost-effective processing method.
• The Sal de Vida process design is approximated from previously completed Allkem operated Olaroz Project test work, results and performance. The Olaroz process design has been successfully proven to produce lithium carbonate since 2015.
• Modifications to the Olaroz process technology mean that salts will be drained and harvested in all ponds. Transfer pumps will be used to transfer concentrated brine from a lower grade pond into a higher-grade pond. A second liming stage will be installed to maximise magnesium ion removal before brine enters the production facilities and an ion-exchange stage will be installed to remove remaining calcium and magnesium ions before precipitating battery grade lithium carbonate.
• Lithium Carbonate is sold as both battery and technical grade product, depending on the concentration of impurities. The project produces both grades of product.
• Pilot testing was conducted during 2020 and 2021; purpose-built pilot ponds and pilot plant validate laboratory test work and explore operational considerations. Future drilled production wells showed a higher concentration grade and lower impurity than pilot testing.
• Deleterious elements have been identified and measurement will be taken to mitigate the risks. Sodium carbonate will be ionized captured before being fed into the crystallisation circuit and magnets will be used to capture are remove impurities related to iron equipment.

• The status of studies of potential environmental impacts of the mining and processing operation. Details of waste rock characterisation and the consideration of potential sites, status of design options considered and, where applicable, the status of approvals for process residue storage and waste dumps should be reported.

• – The project has an approved DIA (Impact Assessment Declaration) from 2014 being the legal instrument to explore, construct and perform exploitation activities. This document is subject and based on a series of commitments and obligations and has been updated every 2 years.

-An Environmental Impact Assessment report is currently underway, with the aim of the Regulatory submission in August 2023 to renewal of the Stage 1 environmental mining permit (DIA).

-A series of approvals and permits relate to environment, chemicals, groundwater and freshwater use, waste management, hazardous and others, are finished and others underway.

• The existence of appropriate infrastructure: availability of land for plant development, power, water, transportation (particularly for bulk commodities), labour, accommodation; or the ease with which the infrastructure can be provided, or accessed.

• The project is located in a flat plain at an altitude of about 4,000m above land surface. The main route to the Project site is from the city of Catamarca via national route 40 to Belen, and provincial Route 43 through Antofagasta de la Sierra to Salar del Hombre Muerto. The road is paved all the way to Antofagasta de la Sierra and continues unpaved for the last 145 km to Salar del Hombre Muerto. The shortest route to the Project site is from Salta via San Antonio de los Cobres. The access road is paved for the first 75 km to San Antonio de los Cobres and continues unpaved for 215 km to Salar del Hombre Muerto. The total distance between the city of Salta and the Sal de Vida Project is 390 km.
• Site infrastructure will consist of the main processing facilities including brine well fields and pumping, evaporation ponds, process plant and waste storage. Allkem’s current operations at the Olaroz Project are of similar nature and process. Internal company policies, standard operating procedures, management systems and structures will allow sufficiently rigid establishment of initial operations at the Project site and reduce commissioning and ramp-up risk.
• The brine production wellfields will be located on two sectors of the Salar de Hombre Muerto, one in the East wellfield for Stage 1 where production will start, and a subsequent stage called the Stage 2 Expansion. This Stage 2 will expand the original area of Stage 1 to the west, south and north. Brine wells will be connected through pipelines to centrally positioned booster ponds. The wells will be equipped with pumps and manifolds to the distribution pipeline.
• The evaporation ponds for Stage 1 will cover 450 ha while the halite evaporation pond of Stage 2 will cover approximately 850 ha while Muriate evaporation ponds for this Stage 2 will cover 50 ha.
• The processing plant will consist of a liming plant to support evaporation pond processes, and a lithium carbonation plant to produce final product. The processing plant will be supported by service infrastructure such as reagents mixing, fuel and storage facility, sulfuric acid preparation, compressors and boilers, water treatment plants and workshops.
• The Project’s accommodation camp will be built next to the process plant area. The camp building will be based on prefabricated material to accommodate up to 900 people. The process facility, support services and accommodation infrastructure are deemed adequate to support the planned facility operation and production rate.
• Electricity for the Plant involves diesel independent generators for electricity and connection to a power line. Shift from diesel generation to natural gas will be available in case natural gas is available for the future. The camp will also have renewable energy.
• The Project support infrastructure has been reviewed and is deemed adequate by the CP to support the processing infrastructure and process operations described in this report.

• The derivation of, or assumptions made, regarding projected capital costs in the study.
• The methodology used to estimate operating costs.
• Allowances made for the content of deleterious elements.
• The derivation of assumptions made of metal or commodity price(s), for the principal minerals and co- products.
• The source of exchange rates used in the study.
• Derivation of transportation charges.
• The basis for forecasting or source of treatment and refining charges, penalties for failure to meet specification, etc.
• The allowances made for royalties payable, both Government and private.

• Capital and operating cost estimates were prepared using AACE International guidelines. The cost estimate was compiled by Allkem management team.
• Commodity price is based on market studies conducted by well-known international consultancy Wood McKenzie.
• Provincial mining royalty is considered based on the mine head value of the extracted ore. In addition, the Federal Argentine government receives an export duty on the FOB while the company exports lithium products.
• Corporate tax rate is set at 35%.
• All estimates disclosed herein are expressed in US dollars. Allkem uses US dollars as reporting currency in all statements and reports. Allkem’s subsidiaries use US dollars as reporting currency and operational currency. Argentine Peso is used as a transactional currency for local payments within the country.
• Transportation charges are estimates based on historical actuals.
• Lithium Carbonate is sold as a final product to end users. The pricing is based upon the projections of production for the three product types, Prime (close to battery grade specification), Purified (exceeds battery grade) and Micronized.

• The derivation of, or assumptions made regarding revenue factors including head grade, metal or commodity price(s) exchange rates, transportation and treatment charges, penalties, net smelter returns, etc.
• The derivation of assumptions made of metal or commodity price(s), for the principal metals, minerals and co-products.

• The lithium cut-off grade set at 300 mg/L is based on a projected LCE price of US$20,000 per tonne.
• During the 40-year Ore Reserve simulation, extracted lithium grades from individual production wells vary between approximately 815 and 520 mg/L due to dilution over the LOM. The average lithium grade of the Proved and Probable Ore reserves corresponds to 757 mg/L and represents the flux-weighted composite brine collected before processing. Extracted grades at individual production wells and the average Proved and Probable Ore reserve concentration are well above the 300 mg/L cut-off grade, demonstrating the production is economically viable.

• The demand, supply and stock situation for the particular commodity, consumption trends and factors likely to affect supply and demand into the future.
• A customer and competitor analysis along with the identification of likely market windows for the product.
• Price and volume forecasts and the basis for these forecasts.
• For industrial minerals the customer specification, testing and acceptance requirements prior to a supply contract.

• Lithium is a commodity with a strong growth profile and increasing demand. The growth trend for Lithium carbonate demand for compound annual growth rate (CAGR) of 14% until 2033 supporting strong market dynamics until at least 2033.
• The company expects to sell the lithium carbonate combing Stage 1 with a 15,000 tpa of production and Stage 2 will incorporate 30,000 tpa more, begin maximum of production 45,000 tpa. Sell considers a combination of long- and short-term contacts, based around forecasts of price provided by industry consultants Wood McKenzie.
• As of the date of this Technical Report, Allkem has no existing formalized commercial agreements in place for the sale of lithium carbonate from the Sal de Vida Project. Allkem remains in discussions with potential customers. In line with the Project execution schedule, these discussions are expected to advance to negotiations throughout the course of the Project.

• The inputs to the economic analysis to produce the net present value (NPV) in the study, the source and confidence of these economic inputs including estimated inflation, discount rate, etc.
• NPV ranges and sensitivity to variations in the significant assumptions and inputs.

• The inputs to the financial model are based on the construction and operating economics parameters for the project and evaluation of deviation from budgeted costs.
• NPV ranges and sensitivity to variations shows that the commodity price has the most significant impact on the Sal de Vida Project’s NPV, followed by production levels, OPEX, and CAPEX. Variation of 10% on Lithium price has an impact of 18% in NPV. This analysis considers only Stage 1.
• Financial considers 100% equity and is reported on a 100% project owner basis.

• The status of agreements with key stakeholders and matters leading to social licence to operate.

• -Allkem has been actively involved in community relations. Although there are minimal inhabitants in the area of the Salar, Allkem has consulted extensively with the local communities and employs members of these communities in the current exploration activities.

              -The company has performed continuous surveys on social perception with local communities, social economics baseline updates, survey of local suppliers and study of local competencies.

              -The company has evaluated positive and negative impacts of the project within the company. Based on social commitments and compliance with local mining authority, SDV has participated in training and improve skills of people from local communities, prioritize the hiring of local operators and technicians in the area of influence, work with the university of Catamarca and technical schools to develop professionals for future positions, consider gender and diversity perspectives in the processes of hiring local labour and in community projects.

• The company has implemented a Community Relations Plan (PRC) between SDV and the communities to develop programs to maximise positive effects of the project and optimize relationship, to minimize the risks of misunderstandings, to encourage families, residents, and institutions to take advantage of sustainable opportunities and to establish an information and consultation system open to the community.
• The company has increased new programs internal procedures to improve community management, has implemented a territorial community management approach and has been developing a Completion of Education with the Ministry of Education of Catamarca. As of March 31, 2022, more than 70% of local employees are from Catamarca and Stage 1 will create approximately 900 full-time positions at peak construction and 170 full-time positions during stable Stage 1 operations.
• Other successful community programs include: Implementation programs of University Technique in Lithium Brine, strengthening program for local rural producers, community medical visits program, community infrastructure program and community infrastructure program.
• Agreements with communities have been set in place, which include internet system installation and hiring of people currently working in various areas of SDV.
• Allkem has a strong commitment to hiring local labour, which favours the socioeconomic development of populations near the SDV Project. The growing activity derived from the construction and operation of the Project will have a positive impact on the revitalization of the local and regional economy. Local communities in the area of influence will be able to access jobs with social benefits, medical services, retirement contributions and good contracting conditions.

• To the extent relevant, the impact of the following on the project and/or on the estimation and classification of the Ore Reserves:
• Any identified material naturally occurring risks.
• The status of material legal agreements and marketing arrangements.
• The status of governmental agreements and approvals critical to the viability of the project, such as mineral tenement status, and government and statutory approvals. There must be reasonable grounds to expect that all necessary Government approvals will be received within the timeframes anticipated in the Pre-Feasibility or Feasibility study. Highlight and discuss the materiality of any unresolved matter that is dependent on a third party on which extraction of the Ore Reserve is contingent.

• For surface rights, SDV is located within fiscal lands owned by the Province of Catamarca with no private land holders. For water rights, the Governor of the Province agrees to grant the relevant water concession. For third parties’ rights, all the mining concessions for the Sal de Vida Project were secured under purchasing agreements with pre-existing owners and claimants.
• Easement acquirements by the company include water, camp, infrastructure and services.
• Presently, Allkem is the operating joint venture partner of the Sales de Jujuy Olaroz lithium carbonate facility and operator of the Mt Cattlin spodumene mine and concentration project.
• As of the date of the reproduction of this JORC Table 1, Allkem has no existing commercial offtake agreements in place for the sale of lithium carbonate from the Sal de Vida Project.
• Allkem’s Galaxy Lithium Sal de Vida S.A. (GLSSA) provides to pay a royalty to the Province of Catamarca based on a Mining Royalty, and Additional Contribution and a CSR Contribution.

• The basis for the classification of the Ore Reserves into varying confidence categories.
• Whether the result appropriately reflects the Competent Person’s view of the deposit.
• The proportion of Probable Ore Reserves that have been derived from Measured Mineral Resources (if any).

• The Ore Reserves are classified as a both Proved and Probable. Projected production wells were all placed in Measured Resource zones.
• Proved Ore Reserves are specified for the first 7 years of operation (years 1-7) in the Stage 1 East Wellfield and years 3-9 for the Stage 2 Expansion Wellfield given that short-term model results have higher confidence due to the current model calibration, and also the initial portion of the projected LOM has higher confidence due to less expected short-term changes in extraction, water balance components, and hydraulic parameters.
• Probable Ore Reserves are conservatively assigned after 7 years of operation (years 8-40 in the Stage 1 East Wellfield and years 10-40 for the Stage 2 Expansion Wellfield) because the numerical model will need to be recalibrated and improved in the future due to potential changes in neighbouring extraction, water balance components, and hydraulic parameters.
• From the point of reference of brine pumped to the evaporation ponds, the Ore Reserves correspond to 0.44 million tonnes of LCE for the Proved Ore category and 2.04 million tonnes of LCE for the Probable Ore category, with a total of 2.48 million tonnes of LCE.
• The total estimated Proved and Probable Ore Reserves represent about 38% of the total Measured and Indicated Resources.
• Given that projected production wells were placed in Measured Resource zones, a majority of the Probable Ore Reserves (approximately 80%) have been derived from Measured Mineral Resources. However, uncertainties in the modifying factors were considered when classifying the Ore Reserves, namely model updates which will be needed as mining progresses.
• The Competent Person (CP) believes that the Proved and Probable Ore Reserves were adequately categorized based on industry standards for lithium brine projects and the reliability of the model projections.

• The results of any audits or reviews of Ore Reserve estimates.

• A preliminary audit was conducted by SRK Consultants in 2022. Minor additional monitoring points were recommended to improve baseline water levels and chemistry.

• Where appropriate a statement of the relative accuracy and confidence level in the Ore Reserve estimate using an approach or procedure deemed appropriate by the Competent Person. For example, the application of statistical or geostatistical procedures to quantify the relative accuracy of the reserve within stated confidence limits, or, if such an approach is not deemed appropriate, a qualitative discussion of the factors which could affect the relative accuracy and confidence of the estimate.
• The statement should specify whether it relates to global or local estimates, and, if local, state the relevant tonnages, which should be relevant to technical and economic evaluation. Documentation should include assumptions made and the procedures used.
• Accuracy and confidence discussions should extend to specific discussions of any applied Modifying Factors that may have a material impact on Ore Reserve viability, or for which there are remaining areas of uncertainty at the current study stage.
• It is recognised that this may not be possible or appropriate in all circumstances. These statements of relative accuracy and confidence of the estimate should be compared with production data, where available.

• In the opinion of the CP, each phase of the Project was conducted in a logical manner, and results were supportable using standard analytical methodologies. In addition, calibration of the numerical model against long-term pumping tests provides solid support for the conceptual hydrogeologic model developed for the Project. Thus, there is a reasonably high-level confidence in the ability of the aquifer system to yield the quantities and grade of brine estimated as Proved and Probable Ore Reserves.
• The estimated Brine Mineral Resources and Brine Ore Reserves summarized in this Report may have upside potential for tonnage increases based on results from the ongoing production well drilling, and aquifer testing of the recently constructed Eastern wellfield production wells.
• Two of the already-drilled production wells have reached bedrock at about 220 meters below land surface (m bls), and one has been drilled to over 300 m bls without reaching bedrock. Previous exploration drilling allowed for a maximum depth of the Brine Resource to about 170 m bls. These deeper drill holes have upside potential to extend the limit of the Brine Resource estimates at depth.
• To the extent known by the CP, there are no known environmental, permitting, legal, title, taxation, socioeconomic, marketing, political or other relevant factors that could affect the
  Ore Reserve estimate which are not discussed.