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Sun Summit's Extensive Data Review Identifies Multiple New High-Grade Gold-Silver Targets at the JD Project

Sun Summit's Extensive Data Review Identifies Multiple New High-Grade Gold-Silver Targets at the JD Project

Sun Summit的廣泛數據審查確定了京東項目的多個新的高品位金銀目標
newsfile ·  05/02 19:00

Vancouver, British Columbia--(Newsfile Corp. - May 2, 2024) - Sun Summit Minerals Corp. (TSXV: SMN) (OTCQB: SMREF) is pleased to announce that it has defined additional targets across the highly prospective Finn to Creek corridor, a significant gold-silver mineralized trend on the recently optioned, road accessible, JD Project in the Toodoggone gold-copper mining district in north-central British Columbia.

不列顛哥倫比亞省溫哥華--(Newsfile Corp.,2024年5月2日)——Sun Summit Minerals Corp.(多倫多證券交易所股票代碼:SMN)(OTCQB:SMREF)欣然宣佈,它已經在極具前景的芬蘭到克里克走廊確定了更多目標,這是最近選擇的不列顛哥倫比亞省中北部Toodoggone金銅礦區京東項目的金銀礦化趨勢。

Highlights:

亮點:

  • Multiple priority drill targets defined through extensive data review: An ongoing comprehensive review and compilation of property-wide historical geochemical data has resulted in the definition of multiple new target areas that warrant considerable follow-up work including drilling.

  • Zones of widespread high-grade gold-silver mineralization: Selected assay highlights* from historical rock samples in the Finn to Creek corridor include:

    • Schmitt Zone: 326 g/t Au with 1,535 g/t Ag (sample 18736) and 64.5 g/t Au with 6,151 g/t Ag (sample 18737)

    • Wolf Zone: 79.2 g/t Au with 30.5 g/t Ag (sample 26070) and 35.4 g/t Au with 44.8 g/t Ag (sample 1710255)

    • MVT Zone: 14.7 g/t Au with 809 g/t Ag (sample 18458) and 11.4 g/t Au with 35.2 g/t Ag (sample 1713456)

    • JD West: 14.8 g/t Au with 910 g/t Ag (sample 1710529) and 14.1 g/t Au with 1,601 g/t Ag (sample 18747)

    • Finn Zone: 47.0 g/t Au with 17.5 g/t Ag (sample VF-24) and 27.3 g/t Au with 61.4 g/t Ag (sample I552528)

  • Broad zones of gold-in-soil anomalism: Gold anomalies, with many samples greater than 1.0 g/t Au, are spatially associated with local zones of outcropping epithermal-related gold-silver mineralization. Many of these coincident anomalies have not been previously drill-tested and represent high-priority areas for future exploration programs.

  • 2024 exploration program currently being finalised: Upcoming field work is anticipated to include geological mapping, soil and rock geochemical surveys, geophysical surveys, as well as significant drilling across multiple targets.

  • 通過廣泛的數據審查定義了多個優先鑽探目標: 對全物業歷史地球化學數據的持續全面審查和彙編已經確定了多個新的目標區域,需要進行包括鑽探在內的大量後續工作。

  • 廣泛的高品位金銀礦化區域: 從芬蘭到克里克走廊的歷史岩石樣本中精選的化驗亮點*包括:

    • 施密特區: 326 g/t Au 含有 1,535 g/t Ag(樣品 18736)和 64.5 g/t Au 和 6,151 g/t Au(樣品 18737)

    • Wolf Zone: 79.2 g/t Au 含有 30.5 g/t Ag(樣品 26070)和 35.4 g/t Au 含有 44.8 g/t Ag(樣品 1710255)

    • MVT 區域: 14.7 g/t Au 含有 809 g/t Ag(樣品 18458)和 11.4 g/t Au 含有 35.2 g/t Ag(樣品 1713456)

    • JD West: 14.8 g/t Au 含有 910 g/t Ag(樣品 1710529)和 14.1 g/t Au 含有 1,601 g/t Ag(樣品 18747)

    • 芬蘭區: 47.0 g/t Au 含有 17.5 g/t Ag(樣品 VF-24)和 27.3 g/t Au 和 61.4 g/t Au(樣品 I552528)

  • 土壤中金異常的廣闊區域: 許多樣品金含量大於 1.0 g/t Au 的金異常在空間上與露出的局部地表熱相關的金銀礦化區域相關。這些重合異常中有許多以前沒有經過鑽探測試,是未來勘探計劃的高度優先區域。

  • 2024 年勘探計劃目前正在敲定: 預計即將進行的實地工作將包括地質測繪、土壤和岩石地球化學調查、地球物理調查以及對多個目標的大量鑽探。

* Assay results are historical and have been compiled from sources believed to be accurate. Grab samples are selective in nature and the resulting assays may not be representative of all mineralization across the project.

* 化驗結果是歷史性的,是根據被認爲準確的來源彙編而成的。採集樣本質上是選擇性的,由此產生的化驗可能無法代表整個項目的所有礦化情況。

"The primary goal of our data compilation effort is to generate walk-up, high-potential drill targets," stated Sharyn Alexander, Sun Summit's President. "Ongoing review of historical data, much of which has never been digital, outlines the presence of outcropping zones of high-grade mineralization from rock samples spatially associated with broad and widespread gold-in-soil anomalies. This coincident relationship provides us confidence to prioritize many of the numerous untested anomalies across the project area, specifically along the Finn to Creek corridor, a highly prospective area of largely untested ground. The fact many of these anomalies are defined by soils samples greater than 1.0 g/t gold strongly supports the high-prospectivity of the targets. Further details of the upcoming field program at JD will be announced as the data compilation efforts come to a close."

太陽峯會主席莎琳·亞歷山大表示:“我們數據彙編工作的主要目標是生成可直接進行的高潛力鑽探目標。”“對歷史數據的持續審查,其中許多數據從來都不是數字化的,這些數據概述了岩石樣本中存在的高品位礦化露頭帶,這些露頭區域與廣泛而廣泛的土壤中金異常有關。這種重合關係使我們有信心優先考慮整個項目區域中衆多未經測試的異常情況,特別是芬蘭到克里克走廊沿線,這是一個前景非常廣闊的地區,基本上未經測試。其中許多異常是由金含量大於1.0 g/t的土壤樣本定義的,這一事實有力地支持了目標的高前景。隨着數據彙編工作的結束,京東即將開展的實地項目的更多細節將公佈。”


Figure 1. JD Project overview


圖 1。京東項目概述

The JD Project comprises over 15,000 hectares of contiguous mineral claims in the prolific Toodoggone gold-copper mining district in north-central British Columbia (Figure 1). The project is host to high-grade, epithermal-related, gold-silver systems and porphyry-related copper-gold systems and lies just north of the Kemess Cu-Au mining camp.

京東項目包括位於不列顛哥倫比亞省中北部多產的圖多貢金銅礦區超過15,000公頃的連續礦產主張(圖1)。該項目擁有高品位、與表熱相關的金銀系統和與斑岩相關的銅金系統,位於Kemess Cu-Au採礦營地以北。


Figure 2. Compiled historical geochemical data from the Finn to Creek gold-silver corridor


圖 2。彙編了從芬蘭到克里克的金銀走廊的歷史地球化學數據

* Compiled historical soil geochemical data has been gridded and contoured. Sample locations are also shown, highlighting only results greater than 1.0 g/t Au.
** Gold assay results from over 540 historical rock samples (grabs from outcrop and float) are shown on the map with select results ranging from 10.6 g/t Au to 326 g/t Au. Grab samples are selective in nature and the resulting assays may not be representative of all mineralization across the project.

*彙編的歷史土壤地球化學數據已經過網格化並勾畫了輪廓。還顯示了樣品位置,僅突出顯示大於 1.0 g/t Au 的結果。
** 地圖上顯示了來自540多個歷史岩石樣本(從露頭和浮標中採集的岩石)的金分析結果,選擇的結果從10.6 g/t金到326克/噸金不等。採集樣本質上是選擇性的,由此產生的化驗可能無法代表整個項目的所有礦化情況。

Target Generation

目標一代

The recent review of surface geochemistry builds on the historical drill data compiled from the Finn and Creek zones (see February 1, 2024 and February 12, 2024 news releases) that anchor each end of the expanded 4.5 km long Finn to Creek gold-silver corridor, host to numerous epithermal-related vein and breccia systems. Priority targets along this corridor, based on surface geochemistry, are as follows.

最近對地表地球化學的審查建立在從芬蘭和克里克地區(見2024年2月1日和2024年2月12日新聞稿)收集的歷史鑽探數據基礎上,這些地帶錨定了長達4.5千米的芬蘭至克里克金銀走廊的兩端,該走廊是許多與地熱相關的礦脈和角礫岩系統的所在地。根據地表地球化學,該走廊沿線的優先目標如下。

Table 1. Selected grab/float (rock) sample highlights from historical exploration programs across the JD project

表 1京東項目歷史勘探項目中的精選抓取/浮動(岩石)樣本亮點

Zone Sample ID Au (g/t) Ag (g/t) UTM_E UTM_N Sample
Wolf 26070 79.2 30.5 609835 6368001 grab
Wolf 1710255 35.4 44.8 609796 6367993 grab
Wolf 1710555 27.3 43.0 609829 6367999 grab
Wolf 26068 16.1 39.0 609835 6367966 grab
Wolf 26069 10.8 33.5 609835 6368001 grab
Tarn 407057 25.6 n/a 610340 6366418 grab
Tarn 26821 10.6 54.4 610127 6366704 grab
Schmitt 18736 326 1535 610121 6368042 float
Schmitt 18737 64.5 6151 610110 6368029 float
Schmitt 18739 49.4 1391 610111 6368060 float
Schmitt 18740 41.1 1297 610071 6368042 float
Schmitt 18738 40.8 3001 610095 6368046 float
Schmitt 1710256 18.9 300 610131 6367979 float
Schmitt 18734 12.7 19.9 610046 6368251 float
MVT 18458 14.7 809 610336 6367556 grab
MVT 1713465 11.4 35.2 610724 6367434 grab
JD West 1710529 14.8 910 610407 6367910 grab
JD West 18747 14.1 1601 610383 6367863 grab
Finn VF-24 47.0 17.5 611146 6367358 grab
Finn I552528 27.3 61.4 611334 6367621 grab
Finn VF-28 18.0 11.8 611013 6367468 grab
Finn VF-25 17.0 9.1 611109 6367385 grab
Finn VF-02 16.5 13.3 611138 6367359 grab
Buff 26818 17.7 47.4 611049 6368377 grab
區域 樣本編號 金 (g/t) 銀 (g/t) UTM_E UTM_N 示例
26070 79.2 30.5 609835 6368001
1710255 35.4 44.8 609796 6367993
1710555 27.3 43.0 609829 6367999
26068 16.1 39.0 609835 6367966
26069 10.8 33.5 609835 6368001
山中小湖 407057 25.6 不適用 610340 6366418
山中小湖 26821 10.6 54.4 610127 6366704
施密特 18736 326 1535 610121 6368042 浮動
施密特 18737 64.5 6151 610110 6368029 浮動
施密特 18739 49.4 1391 610111 6368060 浮動
施密特 18740 41.1 1297 610071 6368042 浮動
施密特 18738 40.8 3001 610095 6368046 浮動
施密特 1710256 18.9 300 610131 6367979 浮動
施密特 18734 12.7 19.9 610046 6368251 浮動
MVT 18458 14.7 809 610336 6367556
MVT 1713465 11.4 35.2 610724 6367434
JD West 1710529 14.8 910 610407 6367910
JD West 18747 14.1 1601 610383 6367863
芬蘭人 VF-24 47.0 17.5 611146 6367358
芬蘭人 I552528 27.3 61.4 611334 6367621
芬蘭人 VF-28 18.0 11.8 611013 6367468
芬蘭人 VF-25 17.0 9.1 611109 6367385
芬蘭人 VF-02 16.5 13.3 611138 6367359
Buff 26818 17.7 47.4 611049 6368377

* Data sources are referenced below.
** Gold assay have been compiled from over 540 historical results from rock samples (grabs from outcrop and float) in the Finn to Creek corridor, with select results from 10.6 g/t Au to 326 g/t Au. Grab samples are selective in nature and the resulting assays may not be representative of all mineralization across the project.

* 下文引用了數據源。
** 金化驗是根據從芬蘭到克里克走廊岩石樣本(從露頭和浮標中採集的)的540多個歷史結果彙編而成的,精選結果從10.6克/噸金到326克/噸金不等。採集樣本質上是選擇性的,由此產生的化驗可能無法代表整個項目的所有礦化情況。

  • Finn - The Finn gold-in-soil anomaly spans 770 metres by 350 metres (Figure 2) and is spatially coincident with previously drill-tested, near-surface epithermal-related gold-silver mineralization (e.g., 35.7 m of 7.3 g/t Au (JD95-047*) and 22.0 m of 12.5 g/t Au (JD95-064*), see February 1, 2024 news release). The relationship between soil geochemical anomalism, up to 12.2 g/t Au, rock chip samples with grades up to 47.0 g/t Au with 17.5 g/t Ag (Table 1), and sub-surface high-grade gold mineralization, suggests that other gold soil anomalies are relatively in-situ. Of the 8 gold-in-soil anomalies identified in this release, only the Finn zone anomaly has been sufficiently drill-tested with reasonably close-spaced drilling.
  • Schmitt - The Schmitt coincident soil and rock geochemical anomaly is centered 1.4 km west of the Finn anomaly (Figure 2). The zone consists of a boulder train of siliceous breccias and banded quartz veins that have historically yielded assays of up to 326 g/t Au with 1,535 g/t Ag, and 64.5 g/t Au with and 6,151 g/t Ag (Table 1). The target has not been adequately drill-tested or trenched (only six short drill holes from the early 1980s), and the bedrock source of the high-grade boulders remains unknown. The Schmitt target is prioritized for systematic follow-up work which may include geological and structural mapping, rock-chip sampling, and follow-up drilling.
  • Wolf - The Wolf gold-in-soil anomaly (up to 8.5 g/t Au), centered 1.6 km west of the Finn zone (Figure 2), is spatially associated with zones of outcropping high-grade gold mineralization reportedly exposed over an area of 90 metres by 50 metres. Gold mineralization is hosted in numerous discrete zones (up to three meters in apparent width) of strongly oxidized hydrothermal breccias and local vein stockwork zones where rock chip samples of up to 79.2 g/t Au with 30.5 g/t Ag, and 35.4 g/t Au with 44.8 g/t Ag have been reported. The Wolf target has not been previously drill-tested and warrants detailed follow up.
  • MVT - The MVT gold-in-soil anomaly is centred 1.0 km west of the Finn anomaly where historical soil sampling defined a strongly anomalous 370 metres by 200 metres target (Figure 2). The soil anomaly (samples up to 5.0 g/t Au) is spatially coincident with grab samples of up to 14.7 g/t Au and 809 g/t Ag (Table 1). The MVT target has not been previously drill tested and represents a priority area for future drill programs.
  • JD West - The JD West gold-in-soil geochemical anomaly covers the gap between the Finn and Schmitt zones (Figure 2) where the potential strike-extension of the prospective, low-angle fault at the Finn zone is locally exposed in historical trenches and has been drill tested in several, widely-spaced, shallow holes (see February 1, 2024 news release). The anomaly is spatially associated with the historical Ag-Carbonate zone where grab sampling from quartz-carbonate breccias, hosted along steeply dipping, north-striking normal faults, yielded up to 14.1 g/t Au with 1,601 g/t Ag (Table 1). Geological mapping focused on examining structural controls is warranted to better define the extent of high-grade gold and silver mineralization across the JD West target.
  • Buff - The Buff gold-in-soil anomaly covers an area just north of the Finn zone, beyond a broad gossan centered on an east-draining creek (Figure 2). Previous drilling at the Buff zone targeted the northern dip-extent of Finn zone mineralization at depth (see February 1, 2024 news release). The presence of soil samples with results up to 1.7 g/t Au, and up to 17.7 g/t Au with 47.4 g/t Ag in rock chip samples, suggests the Buff zone may also host a near-surface gold target north and stratigraphically above and/or offset from the Finn zone. This area therefore warrants geological mapping and rock-chip sampling to better define potential drill targets across the broad anomaly.
  • Creek - The high-grade Creek target, on the western extent of the Finn to Creek corridor (Figure 2), contains poorly defined, structurally controlled high-grade gold mineralization (e.g., 4.0 m at 61.2 g/t Au (CZ97-008*), see February 12, 2024 news release). Soil sampling across the Creek zone with results up to 7.5 g/t Au, and grab samples up to 5.7 g/t Au, suggests the potential for locally concealed and near-surface, gold mineralization. Besides drilling, additional work at the Creek zone will consist of systematic geological and structural mapping and rock-chip sampling. An induced polarization (IP) geophysical survey is also planned across the target area.
  • 芬蘭人 -芬蘭土壤中的金異常跨度爲770米乘350米(圖2),與先前經過鑽探的近地表表熱相關的金銀礦化(例如,35.7米的7.3克/噸金(JD95-047*)和22.0米的12.5克/噸金(JD95-064*),見2024年2月1日新聞稿)。土壤地球化學異常(金含量高達12.2 g/t Au,Ag 17.5 g/t)(表1),以及地下高品位金礦化之間的關係表明,其他金土異常相對較爲原位。在本新聞稿中發現的8個土中金異常中,只有芬蘭地帶的異常經過了足夠的鑽探測試,並進行了合理的近距離鑽探。
  • 施密特 -施密特重合的土壤和岩石地球化學異常位於芬蘭異常以西 1.4 公里處(圖 2)。該區域由一組硅質角礫岩和帶狀石英脈組成,歷來測得的金含量高達326克/噸,銀含量爲1,535克/噸,金含量爲64.5克/噸,銀含量爲6,151克/噸(表1)。目標尚未經過充分的鑽探測試或挖溝(自20世紀80年代初以來只有六個短的鑽孔),高品位巨石的基岩來源仍然未知。施密特目標被優先用於系統的後續工作,其中可能包括地質和結構測繪、岩屑取樣和後續鑽探。
  • -沃爾夫土壤中的金異常(高達 8.5 g/t Au)位於芬蘭地帶以西 1.6 公里處(圖 2),與露出的高品位金礦化區域在空間上相關,據報道暴露在 90 米 x 50 米的區域內。金礦化存在於強氧化熱液角礫岩的衆多離散區域(表觀寬度可達三米)和局部礦脈儲量帶中,據報道,金含量高達 79.2 g/t Au 和 30.5 g/t Au 和 44.8 g/t Au 和 44.8 g/t Au。沃爾夫目標此前未經過鑽探測試,需要進行詳細的後續跟進。
  • MVT -MVT土中金異常位於芬蘭異常以西1.0公里處,歷史土壤採樣確定了370米乘200米的強烈異常目標(圖2)。土壤異常(樣品最高爲5.0 g/t Au)與高達14.7 g/t Au和809 g/t Ag的採集樣品在空間上重合(表1)。MVT 目標之前未經過鑽探測試,是未來鑽探計劃的優先領域。
  • JD West -JD West 土壤中金地球化學異常覆蓋了芬蘭和施密特帶之間的間隙(圖 2),芬蘭地區潛在的低角度斷層的潛在衝擊延伸部分暴露在歷史戰溝中,並已在多個間隔較寬的淺孔中進行了鑽探測試(參見 2024 年 2 月 1 日新聞稿)。該異常在空間上與歷史上的碳酸銀帶相關,在那裏,從石英碳酸角礫岩中採集的樣本位於陡峭傾斜的北向斷層上,得到的金含量高達14.1 g/t,銀含量爲1,601 g/t(表1)。有必要進行以研究結構控制爲重點的地質測繪,以更好地確定京東西部目標地區的高品位金銀礦化程度。
  • Buff -Buff 土壤中的金異常覆蓋了芬蘭地區以北的一個區域,超出了以一條向東排水的小溪爲中心的寬闊的鵝群(圖 2)。此前在Buff區的鑽探目標是芬蘭地帶深度礦化的北部傾斜範圍(見2024年2月1日新聞稿)。土壤樣本的結果高達1.7 g/t Au,岩屑樣本中金含量高達17.7 g/t Ag,這表明Buff區還可能在芬蘭帶以北、地層上方和/或偏離芬蘭帶的近地表金靶點。因此,該區域需要進行地質測繪和岩屑採樣,以更好地確定大異常區域的潛在鑽探目標。
  • 小溪 -位於芬蘭到克里克走廊西部的高品位克里克目標(圖2)包含定義不明確、結構可控的高品位金礦化區(例如,金含量爲61.2克/噸(CZ97-008*)的4.0米,見2024年2月12日新聞稿)。在Creek地區進行土壤採樣,結果高達7.5 g/t Au,採集樣品高達5.7 g/t Au,這表明存在局部隱蔽和近地表的金礦化潛力。除了鑽探外,Creek地區的其他工作還將包括系統的地質和結構測繪以及岩屑採樣。還計劃在目標區域進行感應極化(IP)地球物理調查。

* Note drill intervals are downhole core lengths. True widths are unknown.

* 注意鑽孔間隔是井下岩心長度。真實寬度未知。

These targets, together with targets defined through historical drill data review at the Finn and Creek zones (see February 1, 2024 and February 12, 2024 news release), will form the framework for target prioritization for the upcoming 2024 exploration program, set to commence in early summer. Ongoing data compilation is now focused on merging and re-processing existing airborne and ground geophysical datasets. Details of the upcoming exploration program will be released once compilation efforts are completed and budgets are finalized.

這些目標,以及通過審查芬蘭和克里克地區的歷史鑽探數據確定的目標(見2024年2月1日和2024年2月12日新聞稿),將構成即將到來的2024年勘探計劃的目標優先排序框架,該計劃定於初夏開始。正在進行的數據彙編現在側重於合併和重新處理現有的機載和地面地球物理數據集。即將到來的勘探計劃的細節將在彙編工作完成和預算最終確定後公佈。

National Instrument 43-101 Disclosure

美國國家儀器 43-101 披露

This news release has been reviewed and approved by Sun Summit's Vice President Exploration, Ken MacDonald, P. Geo., a "Qualified Person" as defined in National Instrument 43-101 Standards of Disclosure for Mineral Projects of the Canadian Securities Administrators. He has not been able to verify the historical exploration data disclosed, including sampling, analytical and test data, underlying the technical information in this news release since such data is historical and the original drill core is not readily available. Technical information contained in this release is historical in nature and has been compiled from public sources believed to be accurate. The technical information has not been verified by Sun Summit and may in some instances be unverifiable dependent on the existence of historical drill core and grab samples.

本新聞稿已由Sun Summit的勘探副總裁肯·麥克唐納(P.Geo.)的審查和批准,他是《國家儀器43-101》中定義的 “合格人士” 礦產項目披露標準 加拿大證券管理局的。他無法驗證披露的歷史勘探數據,包括採樣、分析和測試數據,這些數據是本新聞稿中技術信息的基礎,因爲這些數據是歷史數據,而且原始鑽芯不容易獲得。本新聞稿中包含的技術信息本質上是歷史性的,是從被認爲準確的公共來源彙編而成的。技術信息尚未經過 Sun Summit 的驗證,在某些情況下可能無法覈實,具體取決於歷史鑽芯和採集樣本的存在。

Community Engagement

社區參與

Sun Summit is engaging with First Nations on whose territory our projects are located and is discussing their interests and identifying contract and work opportunities, as well as opportunities to support community initiatives. The Company looks forward to continuing to work with local and regional First Nations with ongoing exploration.

Sun Summit正在與我們的項目所在地的原住民接觸,討論他們的利益,確定合同和工作機會,以及支持社區計劃的機會。該公司期待繼續與當地和地區的原住民合作,進行持續的勘探。

About the JD Project

關於京東項目

The JD Project is located in the Toodoggone mining district in north-central British Columbia, a highly prospective deposit-rich mineral trend. The project covers an area of over 15,000 hectares and is in close proximity to active exploration and development projects, such as Thesis Gold's Lawyers and Ranch projects, TDG Gold's Baker-Shasta projects, Centerra's Gold's Kemess East and Underground projects, as well as the past-producing Kemess open pit copper-gold mine.

京東項目位於不列顛哥倫比亞省中北部的Toodogone礦區,這是一個極具前景的富含礦牀的礦產趨勢。該項目佔地超過15,000公頃,緊鄰活躍的勘探和開發項目,例如Thesis Gold的律師和牧場項目、TDG Gold的Baker-Shasta項目、Centerra的Kemess東部和地下項目,以及過去生產的Kemess露天銅金礦。

The project is 450 kilometres northwest of the city of Prince George, and 25 kilometres north of the Sturdee airstrip. It is proximal to existing infrastructure in place to support the past-producing Kemess mine, including roads and a hydroelectric power line.

該項目位於喬治王子城西北450公里處,斯特迪簡易機場以北25公里處。它靠近支持過去生產的凱梅斯礦的現有基礎設施,包括道路和水力發電線。

The JD Project is in a favourable geological environment characterized by both high-grade epithermal gold and silver mineralization, as well as porphyry-related copper and gold mineralization. Some historical exploration, including drilling, geochemistry and geophysics, has been carried out on the property, however the project area is largely underexplored.

JD 項目處於有利的地質環境中,其特徵是高品位的超熱金和銀礦化,以及與斑岩相關的銅和金礦化。已經對該地產進行了一些歷史勘探,包括鑽探、地球化學和地球物理學,但是該項目區域的勘探基本上不足。

About Sun Summit

關於太陽峯會

Sun Summit Minerals (TSXV: SMN) (OTCQB: SMREF) is a mineral exploration company focused on expansion and discovery of district scale gold and copper assets in British Columbia. The Company's diverse portfolio includes the JD Project in the Toodoggone region of north-central B.C., and the Buck Project in central B.C.

Sun Summit Minerals(多倫多證券交易所股票代碼:SMN)(場外交易代碼:SMREF)是一家礦產勘探公司,專注於在不列顛哥倫比亞省擴張和發現區域規模的黃金和銅資產。該公司的多元化投資組合包括位於不列顛哥倫比亞省中北部圖多貢地區的京東項目和位於不列顛哥倫比亞省中部的巴克項目。

Further details are available at .

更多詳情請見。

References

參考文獻

McBride, S. (2013), 2012 Geological, geochemical and diamond drilling report on the JD Property, Assessment Report Indexing System, Report 33556, .

麥克布賴德,S.(2013),《2012年京東地產地質學、地球化學和鑽石鑽探報告》,評估報告索引系統,第33556號報告,。

McBride, S. and Leslie, C. (2014), 2013 Geological, geophysical and diamond drilling report on the JD Property, Assessment Report Indexing System, Report 34762, .

S. 麥克布賴德和萊斯利,C.(2014),《2013年京東地產地質學、地球物理和鑽石鑽探報告》,評估報告索引系統,第34762號報告,。

Morrice, M.G. (1984), 1983 Final Report on the JD Claims Situated Near Moosehorn Creek in the Omineca Mining Division, Project 04, Kidd Creek Mines Ltd., Internal Report.

莫里斯,M.G.(1984),1983年《關於位於奧米內卡礦業部穆斯霍恩溪附近的京東索賠的最終報告》,基德溪礦業有限公司第04號項目,《內部報告》。

Peatfield, G.R. and Schmitt, H.R. (1981), Final Report, 1980 Geological and Geochemical Surveys JD Claims, Omineca Mining Division, B.C., Texasgulf Canada Ltd., Internal Report.

G.R. Peatfield和H.R. Schmitt(1981),《最終報告》,1980年地質和地球化學調查 JD Claims,不列顛哥倫比亞省奧米內卡礦業部,德克薩斯海灣加拿大有限公司,內部報告。

Sutherland, I.G. (1981), Report on Geological and Geochemical Surveys on the JD-81 and Moose-81 Groups Situated at McClair Creek in the Omineca Mining Divisions, Assessment Report Indexing System, Report 9833, .

薩瑟蘭,I.G.(1981),《關於位於奧米內卡礦業部門麥克萊爾溪的 JD-81 和 Moose-81 群的地質和地球化學調查報告》,評估報告索引系統,第 9833 號報告,。

Sutherland, I.G. (1983), 1982 Final Report on the JD Property, Project 04, Kidd Creek Mines Ltd., Internal Report.

薩瑟蘭,I.G.(1983),《1982年京東地產最終報告》,基德溪礦業有限公司,04號項目,內部報告。

Link to Figures

鏈接到數字

Figure 1:

圖 1:

Figure 2:

圖 2:

On behalf of the board of directors

代表董事會

Brian Lock

布萊恩·洛克

For further information, contact:

欲了解更多信息,請聯繫:

Sharyn Alexander
President
info@sunsummitminerals.com

莎琳·亞歷山大
主席
info@sunsummitminerals.com

Matthew Benedetto
Simone Capital
mbenedetto@simonecapital.ca

馬修·貝內代託
西蒙妮資本
mbenedetto@simonecapital.ca

Tel. 416-817-1226

電話 416-817-1226

Forward-Looking Information

前瞻性信息

Statements contained in this news release that are not historical facts may be forward-looking statements, which involve risks, uncertainties and other factors that could cause actual results to differ materially from those expressed or implied by such forward-looking statements. In addition, the forward-looking statements require management to make assumptions and are subject to inherent risks and uncertainties. There is significant risk that the forward-looking statements will not prove to be accurate, that the management's assumptions may not be correct and that actual results may differ materially from such forward-looking statements. Accordingly, readers should not place undue reliance on the forward-looking statements. Generally forward-looking statements can be identified by the use of terminology such as "anticipate", "will", "expect", "may", "continue", "could", "estimate", "forecast", "plan", "potential" and similar expressions. Forward-looking statements contained in this press release may include, but are not limited to, potential mineralization, exploration plans, and engagement with First Nations communities. These forward-looking statements are based on a number of assumptions which may prove to be incorrect which, without limiting the generality of the following, include: risks inherent in exploration activities; the impact of exploration competition; unexpected geological or hydrological conditions; changes in government regulations and policies, including trade laws and policies; failure to obtain necessary permits and approvals from government authorities; volatility and sensitivity to market prices; volatility and sensitivity to capital market fluctuations; the ability to raise funds through private or public equity financings; environmental and safety risks including increased regulatory burdens; weather and other natural phenomena; and other exploration, development, operating, financial market and regulatory risks. The forward-looking statements contained in this press release are made as of the date hereof or the dates specifically referenced in this press release, where applicable. Except as required by applicable securities laws and regulation, Sun Summit disclaims any intention or obligation to update or revise any forward-looking statement, whether as a result of new information, future events or otherwise, except as required by applicable securities laws. All forward-looking statements contained in this press release are expressly qualified by this cautionary statement.

本新聞稿中包含的非歷史事實的陳述可能是前瞻性陳述,其中涉及風險、不確定性和其他因素,這些因素可能導致實際業績與此類前瞻性陳述所表達或暗示的業績存在重大差異。此外,前瞻性陳述要求管理層做出假設,並受固有風險和不確定性的影響。存在很大的風險,即前瞻性陳述無法被證明是準確的,管理層的假設可能不正確,實際業績可能與此類前瞻性陳述存在重大差異。因此,讀者不應過分依賴前瞻性陳述。通常,前瞻性陳述可以通過使用 “預期”、“將”、“預期”、“可能”、“繼續”、“可能”、“估計”、“預測”、“計劃”、“潛力” 等術語和類似的表述來識別。本新聞稿中包含的前瞻性陳述可能包括但不限於潛在的礦化、勘探計劃以及與原住民社區的接觸。這些前瞻性陳述基於許多可能被證明是不正確的假設,這些假設在不限制以下內容的一般性的前提下,包括:勘探活動固有的風險;勘探競爭的影響;意想不到的地質或水文條件;包括貿易法和政策在內的政府法規和政策的變化;未能獲得政府當局的必要許可和批准;市場價格的波動和敏感性;波動性和對資本市場波動的敏感性;通過私募或公開股權融資籌集資金的能力;環境和安全風險,包括監管負擔的增加;天氣和其他自然現象;以及其他勘探、開發、運營、金融市場和監管風險。本新聞稿中包含的前瞻性陳述是截至本新聞稿發佈之日或本新聞稿中特別提及的日期(如果適用)作出的。除非適用的證券法律法規要求,否則除非適用的證券法要求,否則Sun Summit不打算或義務更新或修改任何前瞻性陳述,無論是由於新信息、未來事件還是其他原因。本新聞稿中包含的所有前瞻性陳述均受本警示聲明的明確限制。

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.

多倫多證券交易所風險投資交易所及其監管服務提供商(該術語在多倫多證券交易所風險投資交易所的政策中定義)均不對本新聞稿的充分性或準確性承擔責任。

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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