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    gold investing

    Review of Kilgore 2015-2016 Aspen Corridor Drill Intercepts; Emerging Zone Potential Host to Significant New Gold Mineralization

    Written by Matthew Spizziri
    |
    Feb. 09, 2017 08:48AM PST

    VANCOUVER, BRITISH COLUMBIA–(Marketwired – Feb. 9, 2017) – Otis Gold Corp. (TSXV:OOO) is pleased to present an explanation of significant Tertiary sill- and Cretaceous Aspen Formation-hosted gold intercepts drilled during 2015-2016 at its Kilgore Gold Project, Clark County, ID.

    VANCOUVER, BRITISH COLUMBIA–(Marketwired – Feb. 9, 2017) – Otis Gold Corp. (TSXV:OOO) is pleased to present an explanation of significant Tertiary sill- and Cretaceous Aspen Formation-hosted gold intercepts drilled during 2015-2016 at its Kilgore Gold Project, Clark County, ID. These gold intercepts, which have previously been reported, define a significant, previously unrecognized and under-explored target that collectively delineate a broad zone of gold mineralization, now known as the “Aspen Corridor” (see Aspen Corridor map), which underlies the existing Kilgore Deposit. Dimensions of the corridor, as currently defined by the drill results, are approximately 460-metres-long by 120-metres-wide, and from 60- to 135-metres-thick. Mineralization remains open to the northwest and southeast and at the bottom of many holes. These holes encountered some of the highest gold grades and thickest gold intercepts discovered at Kilgore to date.
    The discovery of this new class of mineralization was subsequent to the discovery of the gold within the current resource estimate for the Kilgore Deposit, the bulk of which is hosted in the overlying Tertiary volcanic rocks. In the 2015 and 2016 drill programs, 34 of 37 holes drilled into the target encountered significant gold mineralization for an overall success rate of 92%. Based upon the results of this drilling, further exploration along the mineralized Aspen Corridor is planned for 2017.
    The Aspen Formation sediment-hosted gold mineralization represents a emerging target on the edge of the Kilgore Volcanic Caldera complex similar to the setting for gold mineralization at the Round Mountain Mine located on the edge of another volcanic caldera complex in Nye County, Nevada and which has produced over 16 million ounces of gold to date. The Aspen mineralization is analogous to Type IV ore at Round Mountain that underlies the caldera-related volcanic pile. The Tertiary Sill unit directly lies between the overlying volcanic rocks (which host the majority of the existing Kilgore Deposit) and the aforementioned Aspen Formation.
    Noteworthy Aspen Corridor intercepts from Otis’ 2015 drilling include:

    • 47.2 m of 2.41 g/t Au in hole 15 OKR-304 (stopped in mineralization)
    • 50.3 m of 4.24 g/t Au in hole 15 OKR-308 (stopped in mineralization)
    • 94.5 m of 4.21 g/t Au in hole 15 OKR-309 (stopped in mineralization)

    Noteworthy Aspen Corridor intercepts from Otis’ 2016 drilling include:

    • 30.5 m of 5.37 g/t Au in hole 16 OKR-315 (stopped in mineralization)
    • 120.4 m of 1.55 g/t Au in hole 16 OKR-318
    • 85.4 m of 2.50 g/t Au in hole 16 OKR-338
    • 69.1 m of 2.07 g/t Au in hole 16 OKR-348 (stopped in mineralization)
    • 120.4 m of 1.18 g/t Au in hole 16 OKC-349
    • 128.0 m of 1.79 g/t Au in hole 16 OKC-353
    • 80.8 m of 1.87 g/t Au in hole 16 OKC-354

    Detailed information relating to these intercepts can be found in Table 1 below and is further detailed in Otis Gold news releases (see News Release dated January 14, 2016 for all 2015 drill results and News Releases dated September 26, 2016, October 31, 2016, November 29, 2016, and January 19, 2017 for 2016 drill results). Note that Table 1 only presents Tertiary Sill and Aspen Formation intercepts (also referred to as “Sill/Aspen”), however many holes listed also contain gold intercepts in the overlying caldera-related volcanic rocks that comprise the majority of the Kilgore Deposit.
    Table 1. Significant 2015 and 2016 Aspen Corridor Intercepts

    Hole
    Number
    Hole
    Type
    TD
    (m)
    Azimuth/
    Angle
    From – To (m)Intercept
    (m)
    Au
    Grade
    (g/t)
    Primary Host
    Rock Unit(s)
    15 OKR-296RC198.1144°/-70°16.8 – 117.3
    161.5 – 173.7
    100.5
    12.2
    0.60
    0.63
    Tertiary Sill
    Aspen
    15 OKR-302RC235.650°/-75°161.5 – 231.670.10.60Tertiary Sill – Aspen
    15 OKR-303RC187.3-/-90°61.0 – 85.324.41.30Tertiary Sill
    15 OKR-304RC222.5-/-90°166.1 – 213.447.22.41Aspen – Tertiary Sill
    15 OKR-307RC243.8230°/-75°167.6 – 195.127.40.83Tertiary Sill
    15 OKR-308RC234.7-/-90°184.4 – 234.750.34.241Aspen – Tertiary Sill
    (Bottomed in mineralization)
    15 OKR-309RC213.450°/-65°118.9 – 213.494.54.212Aspen – Sill – Dike
    (Bottomed in mineralization)
    15 OKR-310RC219.5-/-90°195.1 – 219.524.40.94Aspen
    (Bottomed in mineralization)
    16 OKR-315RC126.5-/-90°96.0 – 126.530.55.37 3Tertiary Sill – Aspen
    16 OKR-316RC182.950°/-77°125.0 – 182.957.90.85Aspen (Bottomed in mineralization)
    16 OKR-317RC182.950°/-75°120.4 – 181.461.01.03Aspen – Tertiary Sill
    (Bottomed in mineralization)
    16 OKR-318RC228.6230°/-80°93.0 – 213.4120.41.554Tertiary Sill and Aspen
    16 OKR-319RC259.0-/-90°195.1 – 227.1
    233.2 – 259.1
    32.0
    25.9
    0.40
    0.51
    Sill and Aspen
    (Bottomed in mineralization)
    16 OKR-320RC283.5-/-90°266.7 – 275.89.10.57Aspen
    16 OKR-323RC173.7-/-90°74.7 – 85.3
    108.2 – 121.9
    132.6 – 140.2
    10.7
    13.7
    7.6
    1.45
    0.53
    0.96
    All in Aspen
    16 OKR-324RC182.9-/-90°93.0 – 158.5
    181.4 – 182.9
    65.5
    1.5
    0.69
    4.00
    All in Aspen (Hole ended in 4.00 g/t Au @ 182.9m)
    16 OKR-325RC219.5-/-90°96.0 – 117.3
    138.7 – 185.9
    21.3
    47.2
    1.27
    0.81
    All in Aspen
    16 OKC-326Core331.6-/-90°89.9 – 105.2
    112.8 – 125.0
    129.5 – 146.3
    160.0 – 198.1
    15.2
    12.2
    16.8
    38.1
    0.68
    0.51
    0.53
    0.81
    All in Aspen
    16 OKC-332Core335.550°/-70°285.0 – 319.434.41.28Aspen
    16 OKC-334Core260.650°/-70°102.1 – 158.0
    185.9 – 208.8
    55.9
    22.9
    0.86
    3.13
    Tertiary Sill
    Aspen
    16 OKC-335Core327.750°/-80°102.1 – 153.951.80.75Tertiary Sill – Aspen
    16 OKR-338RC198.150°/-70°45.7 – 131.1
    176.8 – 195.1
    85.4
    18.3
    2.505
    0.83
    Tertiary Sill and Aspen
    Aspen
    16 OKR-339RC182.950°/-75°96.0-114.3
    153.9=158.5
    18.3
    4.6
    0.75
    0.95
    Tertiary Sill
    Aspen
    16 OKR-342RC213.4-/-90°189.0 – 205.716.70.91Aspen
    16 OKC-344Core298.750°/-65°108.2 – 171.363.10.66Tertiary Sill – Aspen
    16 OKC-345Core299.650°/-70°93.0 – 157.0
    225.6 – 231.6
    64.0
    6.1
    1.08
    2.11
    Breccia – Aspen
    Aspen
    16 OKR-346RC243.8230°/-72°77.7 – 109.7
    134.1 – 138.7
    172.2 – 189.0
    32.0
    4.6
    16.8
    0.89
    0.57
    0.79
    Aspen – Tertiary Sill
    Aspen
    Aspen
    16 OKR-347RC222.5230°/-61°120.4 – 170.750.30.97Aspen
    16 OKR-3486RC174.3230°/-75°80.8 – 97.5
    105.2 – 174.3
    16.7
    69.1
    0.43
    2.077
    Tertiary Sill
    Aspen
    (Bottomed in mineralization)
    16 OKC-349Core322.550°/-80°147.8 – 268.2120.41.18Aspen – Tertiary Sill
    16 OKC-350Core331.650°/-80°196.6 – 207.3
    216.4 – 221.0
    245.4 – 263.7
    10.7
    4.6
    18.3
    0.54
    0.68
    0.46
    Tertiary Sill -Aspen
    Aspen
    Aspen
    16 OK-352Core304.850°/-80°150.9 – 186.8
    195.1 – 219.5
    225.6 – 300.2
    35.9
    24.4
    74.6
    1.12
    0.43
    1.01
    Tertiary Sill – Aspen
    Aspen
    Aspen
    16 ORC-353Core304.8-/-90°164.6 – 292.6128.01.798Tertiary Sill – Aspen
    16 OKC-354Core334.750°/-80°175.3 – 202.7
    240.8 – 321.6
    7.4
    80.8
    1.19
    1.879
    Tertiary Sill – Aspen
    Aspen

    Notes:

    1. Includes 9.1 m @ 12.42 g/t Au
    2. Includes 13.7 m @ 13.46 g/t Au
    3. Includes 13.7 m @ 8.71 g/t Au. This hole has been capped at 34.25 g/t Au (1.0 oz/T)
    4. Includes 3.0 m @ 19.05 g/t Au
    5. Includes 6.1 m @ 12.63 g/t Au
    6. Hole 16 OKR-348 was lost in Aspen Sandstone in rock containing 5.63 g/t Au
    7. Includes 3.0 m @ 14.85 g/t Au
    8. Includes 7.6 m @ 11.96 g/t Au
    9. Includes 7.6 m @ 10.32 g/t Au
    10. True widths are estimated at between 80% and 100% of the drilled interval based on their estimated dip, association with diking, orientation of sedimentary bedding and continuity of mineralization between drill holes.

    Aspen Corridor Cross Section
    A representative cross section (here), the location of which is denoted on the accompanying Aspen Corridor drill hole location map, has been prepared to help the reader better understand the significance of the Aspen Corridor to the Kilgore Deposit and should be reviewed in conjunction with this release.
    Highlights of 2015 and 2016 Aspen Corridor Drill Programs

    1. For the 2015 drilling, 8 of the 9 holes targeting the Sill/Aspen package intercepted mineralization.
    2. For the 2016 drilling, 26 of the 28 holes targeting the Sill/Aspen package intercepted mineralization.
    3. For the 2015-2016 combined drilling, 34 of 37 holes drilled into the Sill/Aspen target encountered significant mineralization for an overall success rate of 92%.
    4. Results of Otis’ 2015-2016 drill campaigns support the premise that gold mineralization in the Aspen Formation is more extensive than indicated by previous drill testing and appears to lie along a northwesterly-trending belt or corridor in the northern half of the Kilgore Deposit, much of which remains open for further drilling.
    5. Results of drill holes targeting the basement Aspen Formation host rocks continue to reveal the presence of significant open-ended mineralization that is typically higher-grade and displays thicker mineralized intercepts than those comprising the current bulk of the Kilgore Deposit in the overlying volcanic host rocks.
    6. Reported intercepts in basement Aspen Formation rocks demonstrate that mineralization exists to depths of up to 300-metres below the surface of the Kilgore Deposit, with some still open at depth.
    7. The Tertiary intrusive sill, which directly overlies the Aspen Formation and locally intrudes the upper portion of it, is also a host to significant mineralization and the extensive contact between the two rock units is an important site for locating additional mineralization in the basement. Significant intercepts can and do exist in both the Aspen Formation and the sill, and in many cases straddle the contact between them to occur continuously throughout both units.
    8. Most of the sill- and Aspen-hosted mineralization in Table 1 is relatively shallow (115- to 130-metres deep) as it occurs in an up-faulted horst block in the northwest half of the Aspen Corridor and is up-faulted and closer to the surface in the southeastern half of the Corridor.

    2015 and 2016 Drill Program Background
    In 2015, nine holes were drilled in northern end of the Kilgore Deposit to test for potential mineralization in the sill and Aspen Formation sedimentary rocks underlying the main Tertiary volcanic host rock package (see January 14, 2016 News Release). Eight of the nine holes encountered significant mineralization. In 2016, a 40-hole program was designed to follow-up on the success of the 2015 program. Drill sites were chosen from an updated set of geologic cross sections and long sections containing all historic results through 2015 to further test the target. Based on these sections, drill holes were selected to test mineralization at depth in the Aspen Formation and to infill and define the limits of the current resource. Selected hole locations targeting the Aspen Formation at depth were focused along the Main Road, Segment 1 Road, North Road and “B” Road areas (the location of the previously mentioned drilling completed in 2015).
    All analytical work was performed by ALS Chemex Labs located in Reno, Nevada and Vancouver, British Columbia that have quality management system certification and technical capability accreditation. A 50-gram pulp of all samples was assayed for gold by Fire Assay/AA finish methods. Certified reference materials, duplicates, and blanks were inserted into the sample stream for quality control. Intercepts reported in Table 1 are calculated using a 0.25 g/t Au cutoff grade and may include a few internal waste intervals less than this cutoff. The RC drilling reported in this release was conducted by O’Keefe Drilling, Inc., Butte, Montana, employing a Foremost 650 Reverse Circulation drill rig outfitted with a circulating wet splitter. The core drilling was conducted by Timberline Drilling of Hayden, Idaho employing two rigs, a DE-140 NQ core rig and an LF-90 HQ core rig. The Qualified Person under National Instrument (NI 43-101) Standards of Disclosure for Mineral Projects for this News Release is Paul D. Gray, P. Geo, who has reviewed and approved its technical content.
    Read the full company profile.
    About the Kilgore Gold Project
    The Kilgore Gold Project contains a current NI 43-101 (dated September 12, 2012) Indicated Resource of 520,000 ounces (oz) Au in 27.4 million tonnes at a grade of 0.59 g/t Au and an Inferred Resource of 300,000 oz Au in 20.2 million tonnes at a grade of 0.46 g/t Au (the “Kilgore Deposit”). The Kilgore Deposit is part of an extensive low-sulfidation quartz-adularia epithermal hydrothermal system hosted in Tertiary volcanic rocks and Aspen Formation calcareous siltstone, shale, and sandstone of Late Cretaceous age. Gold mineralization is of the disseminated, bulk-tonnage type similar to that comprising the classic volcanic-hosted gold deposits at Round Mountain, Nevada and McDonald Meadows, Montana. The Kilgore Deposit exhibits attractive metallurgy with excellent gold recovery averaging greater than 80% at 1.5″ crush size based on column leach test results (see Otis News Release dated June 5, 2012). A new NI 43-101 compliant resource estimate is planned for this year to include the newly recognized Sill/Aspen mineralization.
    About the Company
    Otis is a resource company focused on the acquisition, exploration, and development of precious metal deposits in Idaho, USA. Otis is currently developing its flagship property, the Kilgore Gold Project, located in Clark County, Idaho.
    ON BEHALF OF THE BOARD
    “Craig T. Lindsay”
    President and CEO
    Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.
    The forward-looking information contained in this press release is made as of the date hereof, and Otis undertakes no obligation to update publicly or revise any forward-looking information, whether as a result of new information, future events or otherwise, unless so required by applicable securities laws. This news release does not constitute an offer to sell or a solicitation of an offer to sell any securities in the United States. The securities have not been and will not be registered under the United States Securities Act of 1933, as amended (the “U.S. Securities Act”) or any state securities laws and may not be offered or sold within the United States or to U.S. Persons unless registered under the U.S. Securities Act and applicable state securities laws or an exemption from such registration is available.
    Connect with Otis Gold Corp. (TSXV:OOO) to receive an Investor Presentation.

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    GoldInxs Mining

    GoldInxs Mining (INXS:CC)
    INXS:CC

    Investor Insight

    GoldInxs Mining Corp. (TSXV:INXS, OTCQB: INXGF) provides investors with exposure to early-stage gold-copper exploration in British Columbia, leveraging a portfolio of high-potential projects in Tier 1 jurisdictions, within established gold districts, surrounded by strong regional infrastructure and led by an experienced management team committed to accelerating discovery and delivering shareholder value.

    GoldInxs Mining Corp

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    Overview

    GoldInxs Mining Corp. is a discovery-focused mineral exploration company dedicated to identifying and advancing high-potential copper-gold assets in proven geological belts. The Company's strategy centers on acquiring overlooked and underexplored projects with large-scale potential, applying modern exploration techniques to rapidly evaluate targets and unlock shareholder value through discovery.

    The Company’s. common shares started trading on the TSX Venture Exchange in July 2026 under the symbol INXS, positioning itself to capitalize on favorable copper and gold market fundamentals.

    GoldInxs Mining sample rocks

    Copper demand is forecasted to grow steadily through 2030, with the global copper market expected to expand to over US$340 billion by 2030, driven by electric vehicles, renewable energy and infrastructure growth.

    On the other hand, gold continues to provide a safe-haven hedge against policy risks and market volatility, making GoldInxs’ dual focus on copper and gold particularly compelling for investors.

    The Company’s portfolio is anchored by two priority projects: the Fishpot Project in central British Columbia, interpreted as an emerging, large epithermal system with strong infrastructure access and jurisdiction quality as well as early indications of blackwater-style mineralization, and the non-core Millar Project in the prolific B.C Golden Triangle, a district renowned for world-class discoveries. While surrounding deposits attracted billions of dollars in investment, Fishpot received only sporadic historical exploration despite widespread hydrothermal alteration and numerous anomalous gold, silver and copper results. Artemis Gold’s Blackwater Mine has announced tripling production with an intended $1.56B investment, which sits only 65 km from the Fishpot property.

    Backed by a management team with expertise in exploration, project development and capital markets, GoldInxs is positioned to rapidly advance its assets, deliver near-term exploration catalysts and create shareholder value through discovery and strategic growth.

    Company Highlights

    • Mining-friendly jurisdiction: Projects are in British Columbia, which ranked second in Canada and 20th globally in the 2025 Fraser Institute investment attractiveness rankings.
    • Flagship and district-scale assets: Portfolio is anchored by the flagship Fishpot Project (“Fishpot”) in central B.C., showing strong geological indicators of mineralization, blackwater-style mineralization potential and immense exploration upside potential with only 378 meters of historical drilling. Fishpot is strategically located in the same region as Artemis Gold’s Blackwater Mine and Evolution Mining’s optioned Clisbako property.
    • Clear path to 2026 catalysts: GoldInxs secured a drill permit for an upcoming maiden 2,000-metre drill program at Fishpot, near-term exploration programs are designed to define mineralized systems, outline blackwater-style potential and create shareholder value following the completion of a 3D IP survey and drill targeting.

    Key Projects

    Fishpot Project

    GoldInxs Mining Fishpot Project


    Fistpot property

    The Fishpot Project represents the cornerstone asset within the GoldInxs portfolio. Covering up to 5,500 hectares in Central British Columbia, and located ~95 km north of Quesnel, Fishpot hosts a large hydrothermal alteration system that exhibits many of the geological characteristics observed in major epithermal and intrusion-related gold systems throughout the region. Fishpot encompasses five claim blocks, held under an option to acquire 100 percent subject to a 2 percent NSR, representing a significant exploration opportunity in a highly prospective region.

    Fishpot represents a largely untested hydrothermal mineral system where multiple independent exploration datasets, including gold-silver-copper surface geochemistry, alteration and geology, airborne magnetics, 3D IP chargeability/resistivity and identified epithermal-to-potential-porphyry target environments, are converging to define drill targets, despite only 378 metres of historical drilling across two holes.

    Fishpot is situated within the highly prospective Stikine Terrane and is underlain by Hazelton Group volcanic rocks and intrusive units comparable to those associated with several significant deposits in British Columbia. Extensive quartz-sericite alteration, hydrothermal brecciation, pyrite mineralization and multi-element geochemical anomalies support the interpretation of a robust mineralizing system. Fishpot is strategically positioned near active and historical mining operations, including Artemis Gold’s Blackwater Deposit, Newton Gold Project, Capoose and 3Ts Project, underscoring its large-scale discovery potential. Importantly, based on early-exploration results, Fishpot shares several regional geological characteristics commonly associated with Blackwater-style gold systems, including felsic volcanics, strong alteration, pyrite-rich mineralization and gold-silver geochemical associations. Despite the similarities the Company cannot yet make any formal connections to the surrounding properties, nor can they guarantee that such deposits exist on their ground.

    Fishpot Exploration Technology: GoldInxs advanced its Fishpot targeting program by combining a conventional 3D IP survey with emerging Virtual DRILL™ remote-sensing technology as an additional targeting layer, using multiple geological, geochemical and geophysical datasets to refine and prioritize targets ahead of a planned ~2,000-metre drill program.

    Fishpot Drill Permit & Expansion: GoldInxs has received the required drilling permits and expanded Fishpot to 5,509 hectares, positioning the Company to proceed with its inaugural ~2,000-metre modern drill program on a property that has seen very limited historical drilling, while refining targets through integrated geological, geochemical and geophysical data.

    Despite multiple encouraging exploration indicators, Fishpot has been subjected to only two historic drill holes totaling 378 metres, leaving the broader mineral system largely untested and providing significant leverage to future exploration success.

    Recent exploration completed by GoldInxs generated the highest reported gold value on Fishpot to date, returning up to 5.65 g/t Au from surface sampling, while airborne geophysical surveys identified multiple coincident magnetic and geochemical anomalies that have strengthened the Company's exploration model and target pipeline.

    The 2025 program returned rock samples of up to 5.65 g/t Au, 11.35 g/t Ag and 0.42% Cu, while historical work reportedly returned up to 4.36 g/t Au and 3.2% Cu.

    The property exhibits the potential low-sulphidation epithermal targets at Fishpot North, intermediate-sulphidation signatures at Fishpot East, and a large central magnetic high being evaluated for potential porphyry mineralization at depth. The Company is focused on finalizing drill targeting and preparing for the inaugural diamond drill campaign at Fishpot in the coming months following completion of the IP survey. GoldInxs is preparing to drill-test a 5,509-hectare, largely undrilled hydrothermal system in central British Columbia where high-grade surface gold-silver-copper results, Blackwater-style geological characteristics and multiple coincident geophysical targets have converged to define a portfolio of high-priority exploration targets.

    Management Team

    Nick Michael – President and CEO

    Mr. Michael is a veteran mining executive and technical director with over 37 years of global experience spanning mine development, engineering and operational leadership. His expertise covers the full project lifecycle, including design, construction, technical due diligence and Independent Engineer assignments for institutional investors and project financiers. He also leads CJK Milling, a company focused on reprocessing historical mine waste to recover discarded gold decades ago, when it was less valuable.

    Carlo Rigillo, CPA, Chief Financial Officer

    Mr. Rigillo is an experienced Chartered Professional Accountant with over two decades of experience. He holds a Bachelor of Commerce from the University of Toronto.

    Barry Miller – Executive Chairman and Director

    Mr. Miller brings over 30 years of experience in public markets, including roles as a broker, consultant and financier. He is the founder of GoldInxs and has been actively involved in the resource sector through leadership positions, including as director of Tinova Resources Corp., an exploration company focused on tin and rare earth elements in British Columbia and Alaska.

    Tara Asfour - Vice President, Corporate Development and Communications

    An executive consultant with over 13 years of experience, Tara Asfour holds expertise in corporate development, capital markets, investor relations and strategic communications. She has led strategic financings, partnerships and offtake initiatives within the resource sector through previous corporate development and investor relations roles with multiple publicly listed companies.

    Al Fabbro – Director

    With over three decades of experience spanning both the mining and finance sectors, Mr. Fabbro previously led Yorkton Securities’ retail trading department and was part of its Natural Resources Group. He later served as Lead Director of Roxgold Inc. and currently holds executive leadership roles in the mining industry.

    Darcy Vis, P.Geo. – VP Exploration and Director

    Mr. Vis is an economic geologist with over 17 years of experience in mineral exploration. He has held senior technical roles across multiple exploration companies and is the President of Tripoint Geological Services Ltd. His expertise includes target generation, project evaluation and exploration program execution.

    Stephen Soock, P.Eng., CFA – Director

    Mr. Soock is a mining professional with nearly 20 years of experience spanning both technical operations and capital markets. He currently serves as Vice President, Investor Relations and Development at Heliostar Metals.

    Christopher Kelly, PQS, FCIArb – Director

    Mr. Kelly has over 15 years of experience in construction and natural resources. He holds a BSc in Construction Economics and Management and an MSc in Construction Law and Dispute Resolution, and runs Trachtala Consulting Ltd.

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