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31 st January 2019 Caranbirini Zinc Project, NT Drilling and Joint Venture Update Two out of three high-priority targets successfully drilled. Zinc grades of up to 18.5% in sphalerite encountered over narrow widths in brecciated quartz/carbonate veins in drill-hole CPDH007 at Target A. The hole was terminated at 1,198.8m in Barney Creek Formation above the target horizon (see Figure 1). Hole CPDH006 (Target B) passed through small accumulations of sphalerite, galena and chalcopyrite and 500m of carbonaceous siltstone with laminated pyrite, testing the entire prospective Barney Creek Formation to an end-of-hole depth of 1,127.7m Marindi Metals Limited (ASX: MZN) is pleased to provide an update on drilling activities completed towards the end of 2018 at the Caranbirini Zinc Joint Venture Project in the Northern Territory. As part of its joint venture with Japan Oil, Gas and Metals National Corporation (JOGMEC), Marindi successfully drilled two out of three planned diamond drill-holes into the highly-prospective McArthur Group sedimentary sequence, host to, and less than 10km from the world-class McArthur River zinc-lead operation, owned and operated by Glencore Plc (see Figure 2). Both holes were drilled to final depth of over 1,000m to fully test the CSIRO geophysical interpretation and stratigraphic sequence over Targets A and B. Target J could not be tested due to the discovery and notification of a broad area of native title significance over the planned collar position just prior to drilling. Figure 1. 0.5m @ 18.5% Zn in sphalerite intercept from 284.4m in CPDH007 over Target A. Drilling was completed on-time and within budget. Diamond core was logged and cut and dispatched to the laboratory for analysis prior to Christmas. Given the large amount of core involved, assay results were only received recently. A summary of assays is provided in Table 1 below, and drill-hole collar information is provided in Table 2. Marindi Metals Ltd ASX: MZN Level 3, 35 Havelock St West Perth, WA, 6005 T +61 8 9322 2338 info@marindi.com.au www.marindi.com.au

Page 2 of 9 Hole ID From To Interval Zn % Pb % Cu % Ag % CPDH007 214.82 215.42 0.6 7.62 0.00 0.10 1.00 CPDH007 284.40 284.90 0.5 18.55 0 0 2.00 CPDH007 321.96 322.35 0.39 8.07 0 0 0 CPDH007 928.85 929.85 1 2.13 0 0 0 Table 1. Assay table for drilling at Caranbirini Zinc Project in 2018. Hole ID MGA Easting MGA Northing RL Azimuth Dip EOH Depth CPDH006 615276 8195594 80 085-85 1127.7m CPDH007 612152 8197020 90 040-85 1198.9m Table 2. Collar table for drilling at Caranbirini Zinc Project in 2018. Figure 2. Caranbirini Zinc JV Project target locations. Marindi s Managing Director, Simon Lawson, said: We drilled two drill-holes into this very high-potential area in close proximity to a world-class zinc deposit and intersected the prospective Barney Creek Formation sequence.

Page 3 of 9 At Target A (CPDH007) we intersected a low angle fault system containing high-grade epigenetic zinc sulphides in several brecciated quartz/carbonate veins, but did not reach the lower part of the sequence as it appears to have been faulted down beyond 1,200m depth. Due to the high solubility and mobility of zinc in fault-hosted hydrothermal systems it is our interpretation that the zinc intercepts we see in the fault breccias are evidence of remobilised primary zinc from a nearby large zinc system adjacent the fault system, as shown in Figure 3. At Target B, we drilled the entire Barney Creek Formation sequence and encountered highly carbonaceous sulphidic laminated siltstones, however these lack significant base metal content. Figure 3. Schematic adapted from the Teena zinc deposit stratigraphy illustrating a similar model for fault hosted/remobilised zinc to that seen in CPDH007. Simon Lawson Managing Director and CEO Investor Inquiries Marindi Metals Limited Jeremy Robinson 08 9322 2338 info@marindi.com.au Media Inquiries Read Corporate Nicholas Read 08 9388 1474 nicholas@readcorporate.com.au Competent Persons Statement Information in this release that relates to Exploration Results is based on information prepared by Mr Simon Lawson, a Member of the Australasian Institution of Mining and Metallurgy. Mr Lawson is the Managing Director of Marindi Metals Ltd, a full-time employee and shareholder. Mr Lawson has sufficient experience which is relevant to the styles of mineralisation and types of deposits under consideration and to the activities being undertaken to qualify as a Competent Person as defined in the 2012 Edition of the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves. Mr Lawson consents to the inclusion in this release of the matters based on his information in the form and context in which it appears.

Page 4 of 9 Appendix 1 JORC TABLE 1 Section 1 Sampling Techniques and Data (Criteria in this section apply to all succeeding sections) Criteria JORC Code Explanation Commentary Sampling techniques Drilling techniques Drill sample recovery Logging Nature and quality of sampling (e.g. 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 (e.g. 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 (e.g. submarine nodules) may warrant disclosure of detailed information. Drill type (e.g. core, reverse circulation, open-hole hammer, rotary air blast, auger, Bangka, sonic, etc.) and details (e.g. 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.). 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. 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. Diamond core samples are either NQ2 or HQ in size. Sample intervals are established by a geologist and are determined by geological contacts. Sample intervals are then cut in half and sent to the laboratory. Diamond drill holes have been started with Reverse Circulation drilling using a 5 ½ inch hammer for the upper 100m.Then a section of HQ is drilled, followed by NQ2. Drill holes are routinely surveyed at 30m intervals using a Ranger Discovery Camera survey tool. Orientation measurements are taken at the end of each 6m run using an ACT 3 orientation tool. Drill recovery was 100% for all sample intervals. Geology was logged by experienced Marindi geologists and contract geologists

Page 5 of 9 Subsampling techniques and sample preparation Quality of assay data and laboratory tests Quality of assay data and laboratory tests (Cont d) Verification of sampling and assaying Location of data points Data spacing and distribution Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc.) photography. The total length and percentage of the relevant intersections logged. 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. 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 (e.g. standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (i.e. lack of bias) and precision have been established. 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. 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. 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. All samples were half-cut NQ2 or HQ drill core and were cut with a brick saw. Half core is an appropriate sample size for SEDEX style exploration. ALS laboratory in Perth were used for assaying and the samples were assayed for a full element suite using a 4 acid digest with ICP-MS finish. Where base metal assays were greater than 10000ppm an ore grade ICP-AES finish is used. ALS use high quality control procedures with multiple standards, blanks and duplicates assayed. Marindi also added blanks to be assayed. Significant zinc mineralisation assayed at Caranbirini was first identified visually in the core by contractors and Marindi employees. Zinc mineralisation was then confirmed by portable XRF and later assayed by ALS. A hand held Garmin GPS was used to locate drill collars. The hand held Garmin GPS has an error of +-4m. NA for this release

Page 6 of 9 Orientation of data in relation to geological structure Sample security Audits or reviews Whether sample compositing has been applied. 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 measures taken to ensure sample security. The results of any audits or reviews of sampling techniques and data. The orientation of the drill holes intersects the McArthur Group at a high angle. NA Results have been added to a database and reviewed.

Page 7 of 9 Section 2 Reporting of Exploration Results (Criteria in this section apply to all succeeding sections) Criteria JORC Code Explanation Commentary Mineral tenement and land tenure status Exploration done by other parties Geology Drill hole Information 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. Acknowledgment and appraisal of exploration by other parties. Deposit type, geological setting and style of mineralisation. 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: o easting and northing of the drill hole collar The Caranbirini Project comprises of 8 granted exploration tenements EL28951, EL28952, EL25313, EL28007, EL28006, EL31424, EL25467 and EL29021. All tenements are held by Marindi Metals Ltd. Initial exploration along the Emu fault started in the late 1960 s, and in the early 1970 s the McArthur River Mine was discovered seven kms to the south of Caranbirini. In the 1970 s and 1980 s, Amoco, CRA and Kennnecott completed airborne EM, IP survey, gravity, geochemical assessment and drilling. 7 drill holes were drilled with best results of 0.5m @ 2.5% Pb, 22.4% Zn and 9g/t Ag, and 3m @ 0.9% Pb, 7.3% Zn and 10g/t Ag. In the 1990 s three drill holes were drilled by MIM with best result of 1m @ 1.3% Pb and 17% Zn. Little work was completed in the 2000 s. In 2012 Brumby completed a VTEM survey and tested shallow VTEM anomalies with 4 holes. Only weak Zn anomalism was found. In 2016 Marindi Metals engaged in an Innovation Connections project with CSIRO Mineral Resources. CSIRO used historic drill core, a new gravity survey and the VTEM data to create a 3D structural and geological model. In 2017 Geodiscovery completed a review of the CSIRO work and recommended several priority targets. The Caranbirini Project is located in the McArthur Group on the Emu Fault. The McArthur Basin is divided into the Umbolooga and Batten subgroups. The late-paleoproterozoic Umbolooga subgroup comprises the basal Teena Dolostone, Barney Creek Formation and the Reward Dolostone. The Barney Creek Formation has the Cooley Dolostone Member, the W- fold Shale Member and the HYC Pyritic Shale Member. The Barney Creek Formation hosts the McArthur River Mine with 237Mt @ 13.4% Zn + Pb and the Teena deposit 58Mt @ 12.7% Zn + Pb. See Collar Table in release.

Page 8 of 9 Data aggregation methods Relationship between mineralisation widths and intercept lengths Diagrams Balanced reporting Other substantive exploration data Further work o elevation or RL (Reduced Level elevation above sea level in metres) of the drill hole collar o dip and azimuth of the hole o down hole length and interception depth o 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. In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (e.g. 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. 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 (e.g. down hole length, true width not known ). 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. 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. 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. The nature and scale of planned further work (e.g. tests for lateral extensions or N/A to this release The relationship between mineralisation widths and intercepts is unknown due to lack of drill density. N/A The accompanying document is considered to represent a balanced report. Other exploration data collected is not considered as material to this document at this stage. Further data collection will be reviewed and reported when considered material. N/A to this release

Page 9 of 9 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.