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Jaxon Samples up to 29.69% Antimony at Kispiox Mountain

Jaxon Samples up to 29.69% Antimony at Kispiox Mountain

Jaxon在基斯皮奧克斯山採集的銻含量高達29.69%
newsfile ·  2022/03/10 22:10

Vancouver, British Columbia--(Newsfile Corp. - March 10, 2022) - Jaxon Mining Inc. (TSXV: JAX) (FSE: 0U31) (OTC Pink: JXMNF) ("Jaxon" or the "Company") is pleased to announce the results from the 2021 soil and rock sampling program at the Kispiox Mountain project on the Hazelton Property. 54 rock samples and 11 soil samples were collected during the 2021 field season (Figure 1, Table 1). A high-grade sample with up to 29.69% antimony was collected from within an 8-10 metre wide sulfide quartz veined mineralized zone. Three sulfide quartz mineralized zones with antimony have been identified in the area.

不列顛哥倫比亞省温哥華-(Newsfile Corp.-2022年3月10日)-Jaxon Mining Inc.(多倫多證券交易所股票代碼：JAX)(證券交易所股票代碼：0U31)(場外交易代碼：JXMNF)(以下簡稱“Jaxon”或“公司”)欣然宣佈哈澤爾頓地產基斯皮奧克斯山(Kispiox Mountain)項目2021年土壤和巖石採樣項目的結果。在2021年田間季節收集了54個巖石樣本和11個土壤樣本(圖1，表1)。在8-10米寬的硫化物石英脈狀礦化帶內採集了含銻29.69%的高品位樣品。該區共發現3條含銻硫化物石英礦化帶。

The Kispiox Mountain project is one of seven copper, polymetallic, porphyry-epithermal targets Jaxon is advancing on its 100% owned 723 km2 Hazelton property, located in northwest British Columbia, approximately 50 km north of Smithers, BC.

Kispiox山項目是Jaxon正在推進的七個銅、多金屬、斑巖-淺成熱液目標之一，該項目位於不列顛哥倫比亞省西北部，位於不列顛哥倫比亞省史密瑟斯以北約50公里處，擁有723平方公里的Hazelton地產。

Key Highlights of the 2021 Rock and Soil Sampling Program at Kispiox Mountain Project:

基斯皮奧克斯山項目2021年巖土採樣計劃的主要亮點：

  • Three high-grade antimony sulfide quartz mineralization outcrops, KS zone 1, KS zone 2 and KS zone 3, have been identified by rock and soil samples (Table 1, Figure 2).
  • A high-grade rock sample (A0027254) with up to 29.69% antimony was collected from an outcrop within an 8-10 m wide sulfide quartz veining mineralized zone (KS zone 1, Figure 3), containing minerals of lead-gray stibnite and yellow valentinite. Four surface weathered outcrop samples (A0027255, A0027282-A0027284) assayed Sb grades from 0.18% to 0.59% (Figure 4, Table 1). The oxidation and weathering of the stibnite minerals on the surface may be responsible for reducing the antimony grade within the surface rock samples.
  • 6 metres of chip samples (A0027274-A0027276, Figure 5) from the second sulfide quartz antimony mineralization zone (KS zone 2) reported an average of 2.52% antimony including a 2-metre massive sulfide zone with 6.48% antimony (Table 1, Figure 6) and multiple narrow sulfide antimony quartz veins from 1 centimetre to 20 centimetres over 4 metres.
  • Three rock samples (A0027277-A0027279) were collected from KS zone 3 and reported Sb assays from 0.77% to 2.76% (Figure 2, Table 1). These rock samples contain typical striated prismatic stibnite crystals (Figure 7).
  • 11 soil samples were collected from between KS zone 1 and KS zone 2 and tested with a handheld XRF analyzer which confirmed a high Sb in soil anomaly within the area (Figure 8).
  • 31 rock geochemical samples show elevated Cu, Mo, As and Sb anomalies (Table 2, Figure 9) for porphyry signatures.
  • 三個高品位硫化銻石英礦化露頭，即KS帶1，KS帶2和KS帶3，已被巖石和土壤樣品識別(表1，圖2)。
  • 從8~10m寬的硫化物石英脈狀礦化帶(KS帶1，圖3)的露頭中採集了含銻29.69%的高品位巖樣(A0027254)，其中含有鉛灰色輝銻礦和黃色釩銻礦。四個地表風化露頭樣品(A0027255、A0027282-A0027284)的銻品位從0.18%到0.59%(圖4，表1)。地表輝銻礦礦物的氧化和風化可能是地表巖樣中銻品位降低的原因。
  • 採自第二硫化物石英銻礦化帶(KS 2區)的6米片狀樣品(A0027274-A0027276，圖5)報告平均銻含量為2.52%，其中包括一個2米長的塊狀硫化物帶，含銻6.48%(圖6)，4米內有多條1釐米至20釐米的狹窄硫化銻石英脈。
  • 三個巖石樣品(A0027277-A0027279)從KS區3採集，報告銻含量從0.77%到2.76%(圖2，表1)。這些巖石樣品含有典型的條紋稜柱狀輝銻礦晶體(圖7)。
  • 在KS區1和KS區2之間採集了11個土壤樣本，並用手持XRF分析儀進行了測試，證實了該地區土壤異常中的高Sb(圖8)。
  • 31個巖石地球化學樣本顯示斑巖特徵的Cu、Mo、As和Sb異常升高(表2，圖9)。

Mr. John King Burns, CEO and Chairman of Jaxon, commented, "The rocks with these high-grade antimony results were taken from the propylitic alteration zone at the top of Kispiox Mountain. These anomalously high Sb grades set up the discoveries of a large antimony deposit and of the deeper porphyry system below. We will conduct further systematic soil and sulfide rock outcrop channel sampling programs and additional ground and remote geophysics in the summer of 2022, if time and budgets allow. The elevated Cu, Mo, Pb, Zn and As and the stibnite mineralization in the strong oxide hornfels are classical indicators of a deeper porphyry system. Our target is the porphyry-epithermal system located below Kispiox's epithermal cap. We are continuously evaluating our integrated geological models, ranking each of our seven porphyry-epithermal targets at Hazelton in terms of size and potential grade. With the current information, Kispiox Mountain porphyry ranks at number four behind the Netalzul Mountain, Red Springs, and Blunt Mountain projects."

Jaxon首席執行官兼董事長約翰·金·伯恩斯(John King Burns)先生評論説， “這些含高品位銻的巖石來自基斯皮奧克斯山頂端的原生蝕變帶。這些異常高的銻品位促成了大型銻礦牀和下面更深的斑巖系統的發現。如果時間和預算允許，我們將在2022年夏天進一步開展系統的土壤和硫化巖露頭渠道採樣計劃，以及更多的地面和遠程地球物理。強氧化角閃巖中銅、鉬、鉛、鋅、砷的升高和輝銻礦的礦化是深部斑巖系統的經典標誌。我們的目標是位於基斯皮奧克斯地下熱帽下方的斑巖-淺成熱液系統。我們正在不斷評估我們的綜合地質模型，根據大小和潛在品位對我們在Hazelton的七個斑巖-淺成熱液目標進行排名。根據目前的信息，基斯皮奧克斯山斑巖排名第四，僅次於內塔爾祖爾山、紅泉和布朗特山項目。


Figure 1. Outline map of geology, mineralization and 2021 sampling area at Kispiox Mountain.


圖1.基斯皮奧克斯山地質、礦化及2021年採樣區概貌圖


Figure 2. Three Sb sulfide quartz mineralization zones (KS zones 1, 2 and 3) at Kispiox Mountain.


圖2.基斯皮奧克斯山的三個銻硫化物石英礦化帶(KS帶1、2和3)。


Figure 3. Up to 29.69% Sb rock sample with stibnite and valentinite within 8-10 metre wide KS zone 1.


圖3.在8-10米寬的KS帶內含高達29.69%Sb的含輝銻礦和釩銻礦的巖樣1。


Figure 4. 8-10 metre wide Sb quartz veining mineralization outcrop (KS zone 1).


圖4.8-10米寬的銻石英脈狀礦化露頭(KS帶1)。


Figure 5. 6 metres of chip samples at KS zone 2 outcrop.


圖5.6米KS 2區露頭的巖屑樣品。


Figure 6. >2 metre-wide massive antimony sulfide (stibnite) at KS zone 2.


圖6.>2米寬的塊狀硫化銻(輝銻礦)位於KS 2區。


Figure 7. Antimony rock sample with typical striated prismatic stibnite crystals at KS zone 3.


圖7.KS帶3號帶典型條紋狀稜柱狀輝銻礦的銻巖樣品。


Figure 8. Strong Sb in soil anomalies at Kispiox Mountain.


圖8.基斯皮奧克斯山土壤異常中的強銻。


Figure 9. Strong Cu and Mo in rock anomalies at Kispiox Mountain.


圖9.基斯皮奧克斯山巖石異常中的強Cu和Mo。

Table 1. Significant Rock Sample Assay Results from Kispiox Mountain

表1.基斯皮奧克斯山重要巖石樣品分析結果

Sample ID Description Ag ppm Au ppm Cu ppm Pb ppm Sb ppm Zn ppm
A0027254 10-15 cm wide vein, antimony, stibnite, massive sulfide 0.7 0.02 95 68 296900 18
A0027255 Composite sample, 10 m wide, hornfels with disseminated sulfides, mainly antimony 1.1 0.03 94 13 3300 36
A0027274 Silicified dacite dyke with quartz veins and stibnite veins, 2m chip sample. Str. fractured. The width of stibnite veins varies from 10cm to 0.5 mm. High grade, containing four wide stibnite veins, 10 cm, 3cm, <1cm, <1cm, and many stibnite veinlets 0.5 <0.01 55 41 64800 70
A0027275 2-meter chip sample, containing three stibnite veins, 5 cm, 3cm, <1cm, and many stibnite veinlets 0.5 <0.01 27 12 9037 37
A0027276 2-meter chip sample, containing one wide stibnite veins, 3cm, and many stibnite veinlets 0.5 <0.01 48 13 1860 75
A0027277 Four parallel quartz-stibnite veins within 2 m width, Strike: 5°, Azimuth: 95°, Dip: 60~65 °. First vein 15 cm wide, 4-meter west of second vein <0.5 <0.005 31 77 27550 741
A0027278 Second vein. 3~5 cm wide, 1.5 m west of third vein <0.5 <0.005 59 52 7678 114
A0027279 Chip sample, including third vein and fourth vein. Third vein: 5 cm, Fourth vein: 10~15cm. Vein interval: 1.5 m. <0.5 <0.005 18 19 12340 55
A0027282 Sb mineralization zone, 8 m wide composed sample with multiple 10-1 cm quartz-sb veins 1.1 0.02 68 38 1833 46
A0027283 <0.5 0.009 52 8 5884 38
A0027284 <0.5 0.022 63 25 1869 51
樣本ID 描述 AG ppm Au ppm 銅ppm PB ppm SB ppm 鋅ppm
A0027254 10-15釐米寬的礦脈，銻，輝銻礦，塊狀硫化物 0.7 0.02 95 68 296900 18
A0027255 複合樣品，寬10米，角質硫化物呈瀰漫狀，主要是銻 1.1 0.03 94 13 3300 36
A0027274 含石英脈和輝銻礦脈的硅化英安巖脈，2m片狀樣品。斯塔爾骨折了。輝銻礦脈的寬度從10 cm到0.5 mm不等。高品位，含四條寬大的輝銻礦礦脈，10釐米，3釐米， 0.5 55 41 64800 70
A0027275 2米片狀樣品，含三條輝銻礦脈，直徑分別為5 cm、3 cm、 0.5 27 12 9037 37
A0027276 2米的片狀樣品，包含一個寬的輝銻礦脈，3釐米，以及許多輝銻礦脈。 0.5 48 13 1860 75
A0027277 4條平行的石英-輝銻礦脈，寬度2m，走向5°，方位95°，傾角60~65°。第一脈寬15釐米，第二脈以西4米 31 77 27550 741
A0027278 第二條靜脈。3~5釐米寬，第三脈以西1.5米 59 52 7678 114
A0027279 芯片樣本，包括第三靜脈和第四靜脈。第三靜脈：5 cm，第四靜脈：10~15 cm。靜脈間距：1.5m。 18 19 12340 55
A0027282 銻礦化帶，8米寬的複合樣品，有多個10-1釐米的石英-銻礦脈 1.1 0.02 68 38 1833 46
A0027283 0.009 52 8 5884 38
A0027284 0.022 63 25 1869 51

Table 2. Rock Geochemical Sample Assay Results at Kispiox Mountain

表2.基斯皮奧克斯山巖石地球化學樣品分析結果

Sample ID Easting Northing Ag
ppm		 As
ppm		 Au
ppm		 Cu
ppm		 Mn
ppm		 Mo
ppm		 Pb
ppm		 Sb
ppm		 Zn
ppm
72451 570381 6136424 1.03 1.6 0.002 95.2 203 7.64 15.2 2.19 19
72452 570420 6136539 0.06 6 <0.001 21.7 364 34.85 2.5 2.03 45
72453 570616 6136591 <0.05 3.7 <0.001 20 720 1.17 2.5 0.48 78
72454 570632 6136526 <0.05 5.2 <0.001 25.4 468 0.55 1.8 0.69 78
72455 570792 6136473 0.08 1.7 0.001 28.3 471 0.93 1.5 0.44 60
72456 570797 6136603 <0.05 1.4 <0.001 14.4 559 0.96 2 0.4 75
72457 570815 6136723 <0.05 1 <0.001 18.8 296 19.63 1.9 0.48 23
72458 569405 6136799 0.07 3.7 <0.001 45.9 740 1.55 3.5 0.35 102
72459 569413 6136891 0.09 4.9 <0.001 50.4 808 0.57 4.6 0.46 109
72461 569425 6137007 <0.05 3.7 0.002 8.2 989 0.61 2.3 0.86 70
72462 569391 6137062 0.09 11.1 <0.001 47.8 639 1.85 3.2 4.4 91
72463 569282 6137015 0.08 8.5 <0.001 17.1 1415 0.77 4.7 0.37 80
72464 569262 6136913 0.05 5.3 <0.001 25 1190 0.98 3.8 0.89 80
72465 570954 6136466 0.08 3.9 0.001 63.5 311 4.24 1.8 0.34 26
72466 570155 6136573 0.06 1.7 <0.001 28.2 491 6.1 1.9 0.65 33
72467 570167 6136596 <0.05 0.9 <0.001 13.2 531 19.8 2 0.5 27
72468 570251 6136500 0.07 9.8 <0.001 71.2 260 4.98 2 52.89 30
72478 569904 6136728 0.06 0.9 <0.005 26.9 318 10.98 3.6 <0.5 32
72479 570008 6136880 0.02 <0.2 0.018 16.5 346 8.79 4.1 <0.5 32
72480 570122 6136799 0.13 1.5 0.006 129 428 66.03 5.9 1 31
72481 570150 6136652 0.03 1.5 <0.005 16.3 459 7.78 3.5 3.6 29
7460 569424 6136915 0.7 37 0.01 25 752 2 10 4 73
樣本ID 東距 北距 銀
百萬分之		 AS
百萬分之		 Au
百萬分之		 CU
百萬分之		 錳
百萬分之		 莫
百萬分之		 鉛
百萬分之		 某人
百萬分之		 鋅
百萬分之
72451 570381 6136424 1.03 1.6 0.002 95.2 203 7.64 15.2 2.19 19
72452 570420 6136539 0.06 6 21.7 364 34.85 2.5 2.03 45
72453 570616 6136591 3.7 20 720 1.17 2.5 0.48 78
72454 570632 6136526 5.2 25.4 468 0.55 1.8 0.69 78
72455 570792 6136473 0.08 1.7 0.001 28.3 471 0.93 1.5 0.44 60
72456 570797 6136603 1.4 14.4 559 0.96 2 0.4 75
72457 570815 6136723 1 18.8 296 19.63 1.9 0.48 23
72458 569405 6136799 0.07 3.7 45.9 740 1.55 3.5 0.35 102
72459 569413 6136891 0.09 4.9 50.4 808 0.57 4.6 0.46 109
72461 569425 6137007 3.7 0.002 8.2 989 0.61 2.3 0.86 70
72462 569391 6137062 0.09 11.1 47.8 639 1.85 3.2 4.4 91
72463 569282 6137015 0.08 8.5 17.1 1415 0.77 4.7 0.37 80
72464 569262 6136913 0.05 5.3 25 1190 0.98 3.8 0.89 80
72465 570954 6136466 0.08 3.9 0.001 63.5 311 4.24 1.8 0.34 26
72466 570155 6136573 0.06 1.7 28.2 491 6.1 1.9 0.65 33
72467 570167 6136596 0.9 13.2 531 19.8 2 0.5 27
72468 570251 6136500 0.07 9.8 71.2 260 4.98 2 52.89 30
72478 569904 6136728 0.06 0.9 26.9 318 10.98 3.6 32
72479 570008 6136880 0.02 0.018 16.5 346 8.79 4.1 32
72480 570122 6136799 0.13 1.5 0.006 129 428 66.03 5.9 1 31
72481 570150 6136652 0.03 1.5 16.3 459 7.78 3.5 3.6 29
7460 569424 6136915 0.7 37 0.01 25 752 2 10 4 73

About the Kispiox Mountain Project

關於基斯皮奧克斯山項目

The Kispiox Mountain project is located approximately 16 km northwest of New Hazelton, BC and 70 km northwest of Smithers, BC. It is one of seven projects 100% owned by Jaxon (Figure 10).

基斯皮奧克斯山項目位於不列顛哥倫比亞省新黑茲爾頓西北約16公里處，距不列顛哥倫比亞省史密瑟斯西北約70公里。它是Jaxon 100%擁有的七個項目之一(圖10)。


Figure 10. Jaxon's seven projects on the Hazelton property near Smithers, BC.


圖10.Jaxon在不列顛哥倫比亞省史密瑟斯附近的Hazelton地產上的七個項目。

Historical Works

歷史著作

Limited historical work has been carried out at the Kispiox project area with only one MINFILE on record, the "Date showing". The Date showing is located on the southeast flank of Kispiox Mountain, 19 kilometres northwest of Hazelton. The area is underlain by sedimentary rocks of Late Jurassic Bowser Lake Group, intruded by a small granodiorite body of the Late Cretaceous Bulkley intrusions. Noranda Exploration carried out exploration activities on the Date showing area owing to anomalous molybdenum contents in silt samples and trace chalcopyrite observed in the field. Geological and geochemical surveys on the Date showing area were conducted in 1981 and 1983. 195 soil samples and six rock samples were collected and analyzed in 1981, and 18 rock samples were collected and assayed in 1983. Anomalous Au, Ag, Cu, Mo, Pb and Zn were found in various rock and soil samples. Due to the rugged nature of the terrain, the exploration work was limited in extent (P. McCarter, 1981 and Delbert Myers, 1983). There has been no trenching or drilling at the Kispiox area.

在Kispiox項目區進行了有限的歷史工作，記錄在案的只有一個Minfile，即“日期顯示”。日期顯示位於基斯皮奧克斯山的東南側，在黑茲爾頓西北19公里處。該地區下伏着晚侏羅世鮑瑟湖羣的沉積巖，受到晚白堊世Bulkley侵入體的小型花崗閃長巖體的侵位。由於在現場觀察到淤泥樣品中鉬含量異常和微量黃銅礦，諾蘭達勘探公司在日期顯示區進行了勘探活動。日期顯示區的地質和地球化學調查分別於1981年和1983年進行。1981年採集了195個土樣和6個巖樣，1983年採集了18個巖樣。在各種巖土樣品中均發現異常的Au、Ag、Cu、Mo、Pb、Zn元素。由於地形崎嶇，勘探工作的範圍有限(P.McCarter，1981和Delbert Myers，1983)。Kispiox地區沒有挖溝或鑽探。

Geology

地質學

The Kispiox project is underlain by a series of sedimentary strata of the Late Jurassic Bowser Lake Group and Lower Cretaceous Kitsuns Creek Formation of Skeena Group intruded by numerous Late Cretaceous porphyritic intrusions of Bulkley Plutonic Suite.

Kispiox項目下伏有晚侏羅世Bowser湖羣和Skeena羣下白堊統Kitsuns Creek組的一系列沉積地層，並受到Bulkley深成巖套的大量晚白堊世斑巖侵入體的侵襲。

Mineralization

礦化

The associated quartz-sulfides veins are centered on the area most abundant with intrusive rocks, and the veins are most prevalent along the margins of the intrusions and sheared contact zones (P. McCarter, 1981). A great amount of stibnite was observed in the veins, and trace amount of very fine-grained chalcopyrite and molybdenite appear within and adjacent to the veins. The sulfides are mostly fine-grained and disseminated in the veins. Pyrite is common in the quartz veins, and as fracture coating in the hornfels.

伴生的石英-硫化物礦脈集中在侵入巖最豐富的地區，沿侵入巖和剪切接觸帶的邊緣最常見(P.McCarter，1981)。在礦脈中觀察到大量的輝銻礦，礦脈內和脈旁有微量的極細粒黃銅礦和輝鉬礦。硫化物大多是細粒的，散佈在礦脈中。黃鐵礦在石英脈中很常見，在角質巖層中作為裂隙覆蓋層。

Taking into consideration the widespread rusty pyritic zone, intrusive dykes and plugs, mineralized quartz veins and anomalous Cu, Mo and Sb rock geochemical values, it is evident a porphyry-epithermal Sb-Cu-Mo system exists at the Kispiox project.

考慮到廣泛的生鏽黃鐵礦帶、侵入的巖牆和巖塞、礦化的石英脈和異常的Cu、Mo、Sb巖石地球化學值，Kispiox項目顯然存在斑巖-淺成熱液Sb-Cu-Mo系統。

Rock and Soil Sampling and Analytical Procedures

巖土取樣和分析程序

All samples described in the 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, then securely closed for transport to the Company's secure cold storage locked facility in Smithers, B.C. MSALABS of 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. Laboratory standards and QA - QC are monitored by the Company.

新聞稿中描述的所有樣品均由公司合格的專業地質學家收集。芯片和勘探樣品是由經驗豐富的專業地質人員在野外採集的，他們從露頭或芯片樣品中挑選手部樣品。對樣本進行編號、描述和現場定位，以便進行隨訪。編號的巖石樣品標籤被放置在每個袋子裏，然後牢固地關閉，以便運輸到該公司位於不列顛哥倫比亞省蘭利市史密瑟斯的安全冷藏鎖定設施，在從史密瑟斯安全運輸後收到米袋發貨。樣品是通過粉碎、研磨和粉碎成紙漿，在粉碎和粉碎階段在每個樣品之間洗滌貧瘠的物質來製備的。34種元素用20g礦漿進行ICP-230測定，48種元素用IMS-231測定，金用Fas-111火試金用ICP-ES塗飾法測定，礦石品位用MET-440測定。實驗室標準和QA-QC由公司監督。

Soil samples were taken randomly among the mineralization zones. 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 X-Ray Fluorescence Analyzer) for Cu, Pb, Zn, Ag, Mo, Sb and W.

在礦化帶中隨機抽取土壤樣品。在距地表約25-30釐米的深度對大約200克至300克土壤進行了取樣。在適當的情況下，土壤採樣主要針對B層，樣本被收集在貼有標籤的工藝紙袋中。用pXRF(便攜式X射線熒光分析儀)分析土壤樣品中的銅、鉛、鋅、銀、鉬、銻和鎢。

All work was conducted by the Company's team of qualified geologists.

所有工作都是由該公司合格的地質學家團隊進行的。

Qualified Person

合格人員

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.

Jaxon礦業公司總裁兼首席地質師郭穎婷(Tony)Geo.是National Instrument 43-101定義的合格人員，已審核和準備了本新聞稿中包含的科技信息，並核實了支持該科技信息的數據。

About Jaxon Mining Inc.

關於Jaxon礦業公司

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 700 km2 in 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擁有豐富的大型地質目標/資產，在其100%控制的Hazelton地產上有7個斑巖系統目標，這是一個相互關聯的特許權網絡，位於加拿大不列顛哥倫比亞省西北部的斯基納拱門(Skeena Arch)，佔地700平方公里。斯基納拱門是一個特殊的造山和成礦環境，在年代學上適合保存斑巖的存在。

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.

Jaxon致力於發現更深、更深、更隱蔽、商業規模和品位的Cu、Au、Ag、多金屬斑巖淺成熱液系統，這些系統與更靠近地表的遠端礦化、快速蝕變帶有關。Jaxon的團隊由經驗豐富的模型驅動的探索者組成。收集和整合地球化學、地球物理和構造數據以生成3D模型，以幫助可視化和投影目標斑巖系統的位置。

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.

內塔爾祖爾山是賈克森公司最先進的目標，是黑茲爾頓已確定的7個斑巖熱系統目標中的優先目標。紅泉是準備進行鑽探測試的第二個目標。其他五個目標正處於不同的勘探推進階段。

ON BEHALF OF THE BOARD OF DIRECTORS

我謹代表董事會

JAXON MINING INC.

Jaxon礦業公司。

"John King Burns"

"約翰·金·伯恩斯"

John King Burns, Chairman

約翰·金·彭斯(John King Burns)，董事長

For more information please contact:

如需更多信息，請聯繫：

Investor Relations

投資者關係

Kaye Wynn Consulting
T: 604-558-2630
TF: 1-888-280-8128
E: info@kayewynn.com

凱伊·韋恩諮詢公司(Kaye Wynn Consulting)
T: 604-558-2630
TF：1-888-280-8128
電子郵箱：info@kayewynn.com

Freeform Communications
T: 604-243-0499
E: enquiries@freeform.com

自由形式通信
T: 604-243-0499
電子郵箱：queries@freform.com

Corporate
T: 604-424-4488
E: info@jaxonmining.com

公司
T: 604-424-4488
電子郵箱：info@jaxonmining.com

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.

本新聞稿可能含有前瞻性信息，不包含歷史事實。前瞻性信息涉及風險、不確定因素和其他因素，這些因素可能導致實際事件、結果、業績、前景和機會與此類前瞻性信息明示或暗示的內容大不相同。本新聞稿中的前瞻性信息可能包括但不限於公司的目標、目標或未來計劃。可能導致實際結果與這些前瞻性信息大不相同的因素包括但不限於該公司提交給SEDAR的公開文件中列出的風險。儘管公司認為在準備本新聞稿中的前瞻性信息時使用的假設和因素是合理的，但不應過度依賴這些信息，因為這些信息僅適用於本新聞稿發佈之日，並且不能保證此類事件將在披露的時間框架內發生，或者根本不會發生。除法律要求外，公司沒有任何更新或修改任何前瞻性信息的意圖或義務，無論是由於新信息、未來事件或其他原因。多倫多證券交易所創業板交易所及其法規服務提供商(該術語在多倫多證券交易所創業板政策中定義)均不對本新聞稿的充分性或準確性承擔責任。

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要查看本新聞稿的源版本，請訪問

譯文內容由第三人軟體翻譯。


以上內容僅用作資訊或教育之目的，不構成與富途相關的任何投資建議。富途竭力但無法保證上述全部內容的真實性、準確性和原創性。
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