Vancouver, British Columbia--(Newsfile Corp. - January 19, 2022) - Jaxon Mining Inc. (TSXV: JAX) (FSE: 0U31) (OTC PINK: JXMNF) ("Jaxon" or the "Company") is pleased to announce it has extended the soil and rock sampling program at the Netalzul Mt project where 120 rock and 409 soil samples were collected from the new areas in the 2021 field season (Figure 1). The samples report up to 3052 g/t silver equivalent including 2915 g/t Ag, 0.39 g/t Au, 0.35% Cu, 2.06% Pb and 0.43% Sb (Table 1). Based on MDRU's Toodoggone report (link), the samples identify a high MPIx (MDRU Porphyry Index) centre area coincident with the target vectors generated by Fathom Geophysics' previous modeling. These surface expressions are a product of the large epithermal porphyry system Jaxon is targeting within Netazul Mt.
38 of the new rock samples were assayed for porphyry geochemical index elements and the results outline a high MPIx centre which is used to vector in on the location of the centre of the porphyry system. The Netalzul Mt porphyry is marked by geochemical anomalies involving an intense suite of indicator minerals, as well as significant geophysical anomalies, structural controls and an extended propylitic alternation zone populated with multiple, polymetallic high-grade epithermal, sulfide quartz veined zones perforated by monzonite dykes and with visible K-silicate alteration. Jaxon has commenced programming to conduct a definitive drill test of the centre and the mineralized shells of the Netalzul Mt porphyry system in the summer of 2022.
Netalzul Mt is one of seven porphyry system targets on Jaxon's 100% owned Hazelton property in northwestern British Columbia, approximately 50 km north of the town of Smithers.
Highlights of 2021 Rock and Soil Sampling at Netalzul Mt Project
Statement from Chairman and CEO John King Burns
"Netalzul Mt exhibits one of the strongest geochemical anomalies indicating the location of a porphyry system in BC to date and was ranked as Jaxon's priority porphyry target, the first of seven on the Hazelton property, using Fathom Geophysics' comparative porphyry model earlier in 2021."
"Jaxon's primary technical focus in the winter of 2022 is to reprocess all existing geochemical and geophysical datasets, integrate the new data collected in 2021 and regenerate our geological models to show the geometry of and generate more precise locational coordinates for the Netalzul Mt porphyry system. The modelling will be reviewed by Jaxon's geochemical, geophysical and structural advisors as part of a comprehensive drill target vectoring exercise."
"In the spring of 2022, we expect to publish the updated 3D geological model illustrating projections of the Netalzul Mt porphyry system and the specific vectors that each of the ~5 planned, ~1200-metre tests holes will follow."
Figure 1. Soil and rock samples, Netalzul Mt, 2021
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Figure 2. A large and strong Zn anomaly (> 1000 ppm) has been identified in the hornfels at Netalzul Mt.
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Figure 3. MDRU Porphyry Index ratios indicating the footprint of the porphyry mineralization at Netalzul Mt.
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Figure 4. Rock samples (represented by blue diamonds) from mineralized zones at Netalzul Mt.
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Figure 5. Adit 3 (left); one metre chip sample (#72013) from Adit 4 area with Ag grade @ 2915 g/t (right).
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Figure 6. One metre chip sample (A0027300) at Daisy North Contact Zone area with Au grades of up to 7 g/t.
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Figure 7. Monzonite dyke grab sample (72521) with Cu grades of up to 1.47% from the southwest area of Netalzul Mt.
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Figure 8. Conceptual model of epithermal-porphyry system at Netalzul Mt.
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Table 1. Significant Assay Results from Rock Samples at Netalzul Mt in 2021
Sample ID | Description | Au ppm | Ag ppm | Cu ppm | Pb ppm | Sb ppm | Zn ppm | AgEq ppm |
72013 | Breccia QV with tetrahedrite in adit 4 area | 0.39 | 2915 | 3518 | 20600 | 4252 | 738 | 3052 |
72004 | Sulfide QV at Daisy central zone | 1.54 | 1960 | 22750 | 19300 | 10000 | 5768 | 2416 |
A0027292 | 2 m wide polymetallic QV at Daisy central zone | 0.82 | 442 | 5824 | 41400 | 3336 | 23100 | 725 |
A0027300 | 4 QVs ~ 10-40cm each, total 3-4m wide at Daisy Central zone | 7.01 | 49.1 | 5301 | 681 | 39 | 1523 | 613 |
72008 | 2m wide massive sulfide QV veins at adit 3 area | 0.16 | 298 | 2651 | 33600 | 591 | 7040 | 432 |
72035 | Sulfide QV 30cm | 4.41 | 64.7 | 2110 | 1588 | 300 | 315 | 410 |
72007 | Strongly oxidized QV, abundant pyrite and chalcopyrite patches | 0.15 | 93 | 28890 | 56 | 8 | 98 | 395 |
72015 | QV float with chalco-py. and black minerals. | 0.18 | 234 | 11590 | 1557 | 630 | 569 | 372 |
72018 | 50-100cm thick striking 25, dip at 70, str. Py/chalco-py. | 0.70 | 101 | 6242 | 808 | 952 | 1913 | 226 |
72009 | Adit 4 area, QV zone >15m | 0.09 | 147 | 683 | 4528 | 587 | 300 | 183 |
72521 | disseminate monzonite porphyry dyke under a big granodiorite bold in the SW area | 0.07 | 20.2 | 14710 | 68 | 7 | 152 | 172 |
72019 | strongly FeOx altered, 10-15cm wide, ds py | 0.20 | 125 | 1398 | 331 | 167 | 469 | 157 |
A0027298 | QV and granite in the fracture zone | 0.40 | 92 | 1882 | 842 | 1011 | 2672 | 154 |
72041 | QV and Granite with massive chalco-Py and less Py, main QV only 2-3 cm wide | 0.03 | 29 | 11440 | 5 | 5 | 58 | 146 |
A0027316 | QV float on the east valley slope | 0.15 | 111 | 786 | 1268 | 1685 | 74 | 144 |
72006 | Large QV > 50cm in hornfels. it is in contact zone between hornfels and granite, | 0.08 | 63.1 | 1693 | 637 | 615 | 237 | 118 |
72002 | 6 QVs, strongly FeOx altered, locally sulphide, largest one 15-20cm wide, others 2-5cm wide | 0.06 | 79.8 | 595 | 162 | 5 | 16 | 93 |
72521-1 | monzonite dyke with diss sulfide, extension of Monzonite dyke in hole 5 | 0.03 | 40.4 | 2769 | 207 | 98 | 156 | 91 |
72012 | >3m wide QV Breccia zone, QV breccia same as adit 4 | 0.08 | 64.1 | 422 | 484 | 405 | 114 | 80 |
72033 | QV and granite, see Mo, Py and gray color Quartz, see yellow Mo oxidation, total QV zone > 20 meters | 0.13 | 40.1 | 1873 | 360 | 58 | 123 | 76 |
72010 | QV > 5cm, Py/Chalopy in QV group zone > 2m wide | 0.02 | 39.2 | 2834 | 324 | 16 | 142 | 71 |
Rock and Soil Sampling and Analytical Procedures
All samples described in this news release were collected by the Company's Qualified Professional Geologists. Chip and prospecting samples were collected in the field by experienced, professional geological staff who selected hand samples from outcrop or chip samples. The samples were numbered, described and located in the field for follow-up. Numbered rock sample tags were placed inside each bag and securely closed for transport to the Company's secure cold storage locked facility in Smithers, B.C. MSALABS in Langley, B.C. received the rice bag shipments after secure transport from Smithers. Samples were prepared by crushing, grinding and pulverizing to a pulp with barren material washing between each sample at the crush and pulverizing stages. Then 20 g of pulp was used for the ICP-230 for 34 elements or IMS-231 for 48 elements, FAS-111 fire assay for gold with ICP-ES finish and MET-440 for ore grade samples. Overlimit silver is determined by Fire ASSAY 415 method. Laboratory standards and QA - QC are monitored by the Company.
Soil samples were taken on a 50 m by 50 m grid along the mineralization zone. Approximately 200 g to 300 g of soil was sampled at a depth of approximately 25-30 cm from surface. Soil sampling primarily targeted the B horizon where appropriate, and samples were collected in labelled craft paper bags. Soil samples were analyzed via PXRF (Portable Thermo Scientific Niton XL3t GOLDD+ X-Ray Fluorescence Analyzer) for Cu, Pb, Zn, Ag, Mo, Sb and W. All work was conducted by the Company's team of qualified geologists.
Qualified Person
Yingting (Tony) Guo, P.Geo., President and Chief Geologist of Jaxon Mining Inc., a Qualified Person as defined by National Instrument 43-101, has reviewed and prepared the scientific and technical information and verified the data supporting such scientific and technical information contained in this news release.
About Jaxon Mining Inc.
Rich in large-scale geological targets/assets, Jaxon has seven porphyry system targets on its 100% controlled Hazelton property, an interconnected network of concessions spanning 705.7 km2 in the Toodoggone region of the Skeena Arch in northwest British Columbia, Canada. The Skeena Arch is an exceptionally orogenic and metallogenic setting, geochronologically suitable to host preserved porphyries.
Jaxon pursues the discoveries of deeper, under cover, commercial scale and grade Cu, Au, Ag, polymetallic porphyry epithermal systems associated with distal mineralized, propylitically altered zones nearer to surface. Jaxon's team is made up of experienced model-driven explorationists. Geochemical, geophysical and structural data is collected and integrated to generate 3D models to assist in the visualization and projection of the location of targeted porphyry systems.
Netalzul Mt is Jaxon's most advanced target, the priority of seven identified porphyry epithermal system targets at Hazelton. Red Springs is the second target being prepared for drill testing. The five other targets are in various advancing stages of exploration.
ON BEHALF OF THE BOARD OF DIRECTORS
JAXON MINING INC.
"John King Burns"
John King Burns, Chairman
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This news release may contain forward-looking information, which is not comprised of historical facts. Forward-looking information involves risks, uncertainties and other factors that could cause actual events, results, performance, prospects and opportunities to differ materially from those expressed or implied by such forward-looking information. Forward-looking information in this news release may include, but is not limited to, the Company's objectives, goals or future plans. Factors that could cause actual results to differ materially from such forward-looking information include, but are not limited to, those risks set out in the Company's public documents filed on SEDAR. Although the Company believes that the assumptions and factors used in preparing the forward-looking information in this news release are reasonable, undue reliance should not be placed on such information, which only applies as of the date of this news release, and no assurance can be given that such events will occur in the disclosed time frames, or at all. The Company disclaims any intention or obligation to update or revise any forward-looking information, whether as a result of new information, future events or otherwise, other than as required by law. Neither TSX Venture exchange nor its Regulations 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.
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