Aton Announces the Completion of and the First Results From Its RC Exploration Drilling Programme at Abu Marawat
Aton Announces the Completion of and the First Results From Its RC Exploration Drilling Programme at Abu Marawat
VANCOUVER, BC / ACCESSWIRE / October 11, 2023 / Aton Resources Inc. (TSXV:AAN) ("Aton" or the "Company") is pleased to announce the completion of the reverse circulation percussion ("RC") programme drilling at its 100% owned Abu Marawat Concession ("Abu Marawat" or the "Concession"), in the Eastern Desert of Egypt, as well as the first results from the West Garida and Abu Gaharish prospects (Figure 1).
不列顛哥倫比亞省溫哥華/ACCESSWIRE/2023年10月11日/Aton Resources Inc.(多倫多證券交易所股票代碼:AAN)(以下簡稱“Aton”或“公司”)欣然宣佈,在其全資擁有的位於埃及東部沙漠的Abu Marawat特許權(“Abu Marawat”或“特許權”),以及West Garida和Abu Gaharish礦區的第一批勘探結果(圖1),已經完成了反迴圈衝擊波(RC)專案鑽探。
Highlights:
重點:
- 85 holes were drilled, for a total of 11,700m, during the regional exploration RC programme at the West Garida, Abu Gaharish, Semna and Zeno prospects;
- A further 628m was drilled from 3 groundwater exploration holes approximately 20km west of the Hamama project area;
- Significant flows were recorded from the groundwater exploration holes within Nubian Sandstone cover rocks, proving the concept that this unit could provide process water supplies for the planned Hamama West and Rodruin mining projects;
- Significant mineralised intersections from the Abu Gaharish prospect included 9m @ 2.10 g/t Au, 3m @ 4.61 g/t Au and 3m @ 3.27 g/t Au. The gold mineralisation was primarily concentrated in a broadly mineralised envelope at the Gaharish Main Zone;
- Narrow mineralised intersections at West Garida included 2m @ 3.66 g/t Au and 24.3 g/t Ag from Vein #1 and 1m @ 4.00 g/t Au from Vein #3.
- 在West Garida、Abu Gaharish、Semna和Zeno勘探區塊的區域勘探RC方案期間,共鑽了85個孔,總長達11700米;
- 在Hamama專案區以西約20公里處的3個地下水勘探孔中又鑽了628米;
- 從努比亞砂岩覆蓋巖內的地下水勘探孔記錄到大量流量,證明瞭該裝置可以為計劃中的Hamama West和Rodruum採礦專案提供工藝用水的概念;
- Abu Gaharish探礦的重要礦化交匯處包括9米@2.10克/噸金、3米@4.61克/噸金和3米@3.27克/噸金。金礦化主要集中在加哈裡什主帶的寬廣礦化包體中;
- 西加裡達狹窄的礦化交叉點包括來自1號礦脈的2m@3.66 g/t Au和24.3 g/t Ag,以及來自3號礦脈的1 m@4.00 g/t Au。
"We are pleased to announce the successful completion of the regional RC exploration drilling programme at Abu Marawat, and to provide the first tranche of results" said Tonno Vahk, Interim CEO. "We are particularly happy with the results of the groundwater drilling in the Nubian Sandstone west of Hamama, designed to test the potential of these rocks to provide process water supplies to the planned starter heap leach mining project at Hamama West. The results were very encouraging with the drilling intersecting significant groundwater hosted in the Nubian cover. It is particularly encouraging that the drilling did not penetrate deep enough to intersect the main target, the basal Tarif Sandstone Unit of the Nubian, which suggests that this unit may host significant groundwater resources closer to Hamama than was previously anticipated. EMRA continue to review our submission to them detailing Commercial Discoveries at the Hamama West and Rodruin deposits, in accordance with the terms of the Abu Marawat Concession Agreement, and we are hopeful that this process is moving towards a successful conclusion and the issuance of the mining licence at Abu Marawat. The issuance of the first gold mining licence in Egypt to a publicly listed foreign investor since Sukari in 2005 would represent a very significant step forwards for Aton, as well as for Egypt, the Ministry of Petroleum and EMRA."
我們很高興地宣佈,區域資源中心在阿布馬拉瓦特的勘探鑽探計劃已成功完成,並提供了第一批結果。臨時首席執行官託諾·瓦克說。“我們對哈馬以西努比亞砂岩的地下水鑽探結果特別滿意,該鑽探旨在測試這些岩石的潛力,為計劃在哈馬西啟動的堆浸採礦專案提供工藝水供應。鑽探與努比亞蓋層的大量地下水相交,取得了非常令人鼓舞的結果。特別令人鼓舞的是,鑽探沒有深入到與主要目標努比亞的塔裡夫砂岩單元相交的深度,這表明該單元可能擁有大量地下水資源,比先前預期的更接近哈馬島。Emra根據Abu Marawat特許權協定的條款,繼續審查我們提交給他們的詳細介紹在Hamama West和Rodruum礦藏的商業發現的檔案,我們希望這一進程正在朝著成功完成和頒發Abu Marawat採礦許可證的方向邁進。自2005年Sukari以來,埃及向公開上市的外國投資者發放的第一個黃金開採許可證將標誌著Aton以及埃及、石油部和EMRA向前邁出了非常重要的一步。
2023 Abu Marawat RC drilling programme
2023年阿布馬拉瓦特RC鑽井方案
The exploration RC drilling, undertaken by Geodrill's Egyptian branch, Geodrill for Leasing and Specialized Services Freezone LLC, commenced at the West Garida prospect, 3km east of Hamama West. Prior to the rig being mobilised to Abu Gaharish, 3 groundwater exploration holes were also drilled to test the Nubian Sandstone aquifer approximately 20km west of the Hamama project. Drilling at Abu Gaharish, and subsequently at the Semna and Zeno prospects was supported by fly camps. The drill metres for the programme are summarised in Table 1.
勘探RC鑽探由GeoDrill的埃及分公司GeoDrill for Leating and Specialized Services Free Zone LLC進行,從Hamama West以東3公里處的West Garida勘探區塊開始。在將鑽井平臺調動到Abu Gaharish之前,還鑽了3個地下水勘探孔,以測試Hamama專案以西約20公里處的努比亞砂岩含水層。在Abu Gaharish的鑽探,以及隨後在Semna和Zeno的鑽探都得到了蒼蠅營地的支持。該方案的鑽探米匯總在表1中。
Project |
Number of holes |
Total metres |
Groundwater exploration (Nubian Sandstone) |
3 |
628 |
West Garida |
21 |
1,522 |
Abu Gaharish |
22 |
3,300 |
Semna |
21 |
3,662 |
Zeno |
21 |
3,216 |
Total |
88 |
12,328 |
專案 |
孔數 |
總米 |
地下水勘探(努比亞砂岩) |
3. |
六百二十八 |
西加裡達 |
21歲 |
1,522 |
阿布·加哈裡什 |
22 |
3300 |
塞姆納 |
21歲 |
3662 |
澤諾 |
21歲 |
3216 |
總計 |
88 |
12,328 |
Table 1: Breakdown of the RC drilling completed
表1:RC鑽探已完成的細目
Figure 1: Geology and prospect plan of the Abu Marawat Concession
圖1:阿布馬拉瓦特特許權的地質和遠景規劃
Groundwater exploration drilling
地下水勘探鑽探
2 holes HAW-01 and HAW-02 were drilled south of the Hamama access road approximately 20km west of the Hamama West mineral deposit to test the potential of the Nubian Sandstone Formation to produce sufficient volumes of process water for the proposed Hamama West. Hole HAW-03 was drilled approximately 4km further east of HAW-01, back towards Hamama. Details and locations of the holes are provided in Table 2.
在Hamama West礦藏以西約20公里處Hamama通道以南約20公里處鑽探了2個HAW-01和HAW-02孔,以測試Nubian砂岩地層的潛力,為擬建的Hamama West生產足夠數量的工藝水。HAW-03井是在HAW-01以東約4公里處向Hamama方向鑽探的。孔的詳細資訊和位置見表2。
Hole ID |
Collar co-ordinates 1,2 |
EOH depth (m) |
Dip |
Grid azimuth |
Comments |
||
X |
Y |
Z |
|||||
HAW-01 |
517072 |
2910962 |
291 |
100 |
-90 |
- |
Hole dry |
HAW-02 |
516679 |
2909410 |
285 |
294 |
-90 |
- |
c. 700 l/min flow from 270m depth |
HAW-03 |
520792 |
2911753 |
315 |
234 |
-90 |
- |
c. 480 l/min flow from 222m depth |
Notes:
|
孔ID |
領座標系1,2 |
EOH深度(米) |
浸漬 |
柵格方位角 |
評論 |
||
X |
是的 |
Z |
|||||
HAW-01 |
517072 |
2910962 |
二百九十一 |
100個 |
-90 |
- |
井眼幹燥 |
HAW-02 |
516679 |
2909410 |
二百八十五 |
二百九十四 |
-90 |
- |
c.700 L/分鐘水深270米 |
How-03 |
520792 |
2911753 |
315 |
二百三十四 |
-90 |
- |
c.480 L/分鐘222m水深流量 |
備註:
|
Table 2: Collar details of groundwater exploration drill holes
表2:地下水勘探鑽孔的卡箍細部
The RC holes were drilled at 53⁄4" diameter, with holes HAW-02 and HAW-03 reducing to 51⁄2" diameter. Holes HAW-01 and HAW-02 were cased through the surface alluvial sheet wash deposits to 12m depth, and HAW-03 was cased to 30m depth.
RC孔的鑽孔直徑為53⁄4“,其中HAW-02和HAW-03孔的直徑減少到51⁄2”。HAW-01和HAW-02孔穿過表層沖積席狀沉積物至12m處,HAW-03孔至30m處。
Hole HAW-01 failed to intersect any water by its target depth of 100m, and was terminated. Holes HAW-02 and HAW-03 both intersected significant groundwater from about 120m depth, with the drillers unable to keep the holes and samples dry (Figure 2). Hole HAW-02 was terminated at 294m, and HAW-03 was terminated at 234m, due to the hole collapsing in water-bearing sandstones.
HAW-01孔在其目標深度100米處未能與任何水相交,因此被終止。HAW-02和HAW-03兩個孔都從大約120米深的地方與大量地下水相交,鑽探人員無法保持孔和樣品的乾燥(圖2)。由於HAW-02井在含水砂岩中坍塌,HAW-02井在294m處終止,HAW-03井在234米處終止。
All holes were drilled through a variegated sequence of predominantly brown, red, grey and black shales and mudstones, with intercalated sandstone units interpreted as belonging to the Quseir Unit of the Cretaceous Nubian Sandstone Formation. The target basal Tarif Sandstone Unit of the Nubian Sandstone Formation was not intersected in any of the 3 holes.
所有的孔都鑽過了以棕色、紅色、灰色和黑色為主的葉巖和泥岩的雜色序列,夾層砂岩單元被解釋為屬於白堊紀努比亞砂岩建造的Quseir單元。努比亞砂岩組的目標塔裡夫砂岩單元沒有在三個孔中的任何一個相交。
Figure 2: Drilling on groundwater exploration hole HAW-02
圖2:HAW-02地下水探測孔的鑽探
Both holes HAW-02 and HAW-03 started making significant amounts of water from about 120m onwards, with the volume increasing with depth. Water was primarily hosted within sandstone horizons intercalated with the predominantly shale and mudstone sequence. Airlift testing was carried out on both holes, using the booster compressor, but no formal pump testing was undertaken. Water flows were measured using a V-notch weir system. Significant water flows were recorded from both holes HAW-02 and HAW-03, to a maximum of c. 700 l/min from 270m depth, and 480 l/min from 220m depth, respectively.
HAW-02和HAW-03兩個孔從大約120米開始產生大量的水,體積隨著深度的增加而增加。水主要賦存於以葉巖和泥岩為主的層序夾層的砂岩層內。使用增壓壓縮機在兩個孔上進行了氣升測試,但沒有進行正式的泵測試。水流測量採用V型槽堰系統。從HAW-02和HAW-03兩個孔記錄到大量的水流,最大流量為c.在270m深度和220m深度分別為700 L/分鐘和480 L/分鐘。
The programme has successfully proved the concept that the Nubian Sandstone cover which outcrops to the west of the Hamama area could potentially host sufficient groundwater resources to provide process water for the proposed Hamama West open mine and heap leach project. It is noted that the drilling failed to intersect the deeper basal Tarif Sandstone Unit of the Nubian Sandstone Formation that was the primary target of the programme. The Nubian Sandstone cover dips west towards the Nile River basin, which suggests that the Tarif Formation aquifer could be potentially intersected and exploited for groundwater at shallower depths and further east towards the Hamama project, thus reducing the required pumping distance.
該方案成功地證明瞭這樣一個概念,即Hamama地區以西露頭的努比亞砂岩覆蓋層可能擁有足夠的地下水資源,為擬議的Hamama West露天礦山和堆浸專案提供工藝水。據指出,鑽探未能與努比亞砂岩地層更深的塔裡夫砂岩單元相交,該砂岩單元是該方案的主要目標。努比亞砂岩覆蓋層向西向尼羅河流域傾斜,這表明塔裡夫組含水層有可能交叉開採較淺深度的地下水,並進一步向東向Hamama專案開採,從而縮短了所需的抽水距離。
Exploration RC drilling
勘探RC鑽探
West Garida
西加裡達
21 drill holes, WGP-006 to WGP-025, were completed at the West Garida prospect (Figure 1), for a total of 1,522m metres (Table 3 and Figure 3). The mineralisation at West Garida is associated with several narrow shallow-dipping coarse gold-bearing quartz veins, with the drilling designed to follow up on a previous RC drill intersection of 41.7 g/t Au, 263 g/t Ag and 2.08% Pb over a 1m interval in hole WGP-003 (see news release dated September 1, 2022).
WGP-006至WGP-025 21個鑽孔在西加裡達探礦完成(圖1),總長度為1,522米(表3和圖3)。West Garida的礦化與幾個狹窄的淺層粗含金石英脈有關,鑽探旨在跟進之前在WGP-003孔1米間隔內RC鑽探交匯處的41.7克/噸金、263克/噸銀和2.08%鉛(見日期為2022年9月1日的新聞稿)。
Hole ID |
Collar co-ordinates 1,2 |
EOH depth (m) |
Dip |
Grid azimuth |
Comments |
||
X |
Y |
Z |
|||||
WGP-006 |
537327.4 |
2914773.9 |
630.6 |
100 |
-71.3 |
0.8 |
Vein #1 |
WGP-007 |
537327.4 |
2914776.0 |
630.6 |
100 |
-51.3 |
3.1 |
Vein #1 |
WGP-008 |
537327.1 |
2914762.7 |
630.6 |
57 |
-65.0 |
179.6 |
Vein #1 (hole abandoned) |
WGP-008a |
537327.4 |
2914766.2 |
630.6 |
120 |
-64.8 |
181.1 |
Vein #1 (re-drill of WGP-008) |
WGP-009 |
537327.5 |
2914767.1 |
630.7 |
110 |
-78.7 |
180.6 |
Vein #1 |
WGP-010 |
537240.4 |
2914803.6 |
614.7 |
60 |
-48.1 |
1.4 |
Vein #1 |
WGP-011 |
537240.2 |
2914800.3 |
614.9 |
60 |
-89.5 |
351.9 |
Vein #1 |
WGP-012 |
537238.9 |
2914737.2 |
629.7 |
100 |
-55.0 |
358.1 |
Vein #1 |
WGP-013 |
537239.0 |
2914735.6 |
629.8 |
100 |
-74.3 |
1.1 |
Vein #1 |
WGP-014 |
537239.0 |
2914734.6 |
629.9 |
100 |
-90.0 |
0.0 |
Vein #1 |
WGP-015 |
537239.1 |
2914728.3 |
630.1 |
110 |
-80.6 |
189.1 |
Vein #1 |
WGP-016 |
536845.5 |
2914990.0 |
637.6 |
40 |
-89.8 |
221.4 |
Vein #2 |
WGP-017 |
536847.7 |
2914991.3 |
637.7 |
40 |
-50.0 |
59.5 |
Vein #2 |
WGP-018 |
536797.7 |
2914961.8 |
634.3 |
40 |
-50.6 |
58.8 |
Vein #2 |
WGP-019 |
536795.2 |
2914960.6 |
634.2 |
50 |
-89.6 |
335.8 |
Vein #2 |
WGP-020 |
536790.9 |
2914958.3 |
633.9 |
75 |
-55.4 |
237.7 |
Vein #2 |
WGP-021 |
536780.6 |
2915143.5 |
627.5 |
50 |
-50.5 |
129.2 |
Vein #3 |
WGP-022 |
536778.6 |
2915145.1 |
627.4 |
60 |
-89.4 |
147.9 |
Vein #3 |
WGP-023 |
536775.8 |
2915147.1 |
627.3 |
70 |
-59.2 |
311.5 |
Vein #3 |
WGP-024 |
536836.9 |
2914991.5 |
637.2 |
40 |
-50.3 |
315.4 |
Vein #2 |
WGP-025 |
536845.1 |
2914986.0 |
637.6 |
40 |
-50.1 |
179.5 |
Vein #2 |
Notes:
|
孔ID |
領座標系1,2 |
EOH深度(米) |
浸漬 |
柵格方位角 |
評論 |
||
X |
是的 |
Z |
|||||
WGP-006 |
537327.4 |
2914773.9 |
630.6 |
100個 |
-71.3 |
0.8 |
1號靜脈 |
WGP-007 |
537327.4 |
2914776.0 |
630.6 |
100個 |
-51.3 |
3.1 |
1號靜脈 |
WGP-008 |
537327.1 |
2914762.7 |
630.6 |
57 |
-65.0 |
179.6 |
1號脈(已廢棄的洞) |
WGP-008a |
537327.4 |
2914766.2 |
630.6 |
120 |
-64.8 |
181.1 |
1號脈(重鑽WGP-008) |
WGP-009 |
537327.5 |
2914767.1 |
630.7 |
110 |
-78.7 |
180.6 |
1號靜脈 |
WGP-010 |
537240.4 |
2914803.6 |
614.7 |
60 |
-48.1 |
1.4 |
1號靜脈 |
WGP-011 |
537240.2 |
2914800.3 |
614.9 |
60 |
-89.5 |
351.9 |
1號靜脈 |
WGP-012 |
537238.9 |
2914737.2 |
629.7 |
100個 |
-55.0 |
358.1 |
1號靜脈 |
WGP-013 |
537239.0 |
2914735.6 |
629.8 |
100個 |
-74.3 |
1.1 |
1號靜脈 |
WGP-014 |
537239.0 |
2914734.6 |
629.9 |
100個 |
-90.0 |
0.0 |
1號靜脈 |
WGP-015 |
537239.1 |
2914728.3 |
630.1 |
110 |
-80.6 |
189.1 |
1號靜脈 |
WGP-016 |
536845.5 |
2914990.0 |
637.6 |
40歲 |
-89.8 |
221.4 |
2號脈 |
WGP-017 |
536847.7 |
2914991.3 |
637.7 |
40歲 |
-50.0 |
59.5 |
2號脈 |
WGP-018 |
536797.7 |
2914961.8 |
634.3 |
40歲 |
-50.6 |
58.8 |
2號脈 |
WGP-019 |
536795.2 |
2914960.6 |
634.2 |
50 |
-89.6 |
335.8 |
2號脈 |
WGP-020 |
536790.9 |
2914958.3 |
633.9 |
75 |
-55.4 |
237.7 |
2號脈 |
WGP-021 |
536780.6 |
2915143.5 |
627.5 |
50 |
-50.5 |
129.2 |
3號脈 |
WGP-022 |
536778.6 |
2915145.1 |
627.4 |
60 |
-89.4 |
147.9 |
3號脈 |
WGP-023 |
536775.8 |
2915147.1 |
627.3 |
70 |
-59.2 |
311.5 |
3號脈 |
WGP-024 |
536836.9 |
2914991.5 |
637.2 |
40歲 |
-50.3 |
315.4 |
2號脈 |
WGP-025 |
536845.1 |
2914986.0 |
637.6 |
40歲 |
-50.1 |
179.5 |
2號脈 |
備註:
|
Table 3: Collar details of RC exploration drill holes at West Garida
表3:西加裡達RC勘探鑽孔的鑽柱細節
Figure 3: West Garida drill hole collar plan
圖3:西加裡達鑽孔卡箍平面圖
Hole ID |
Intersection (m) |
Assays (ppm) |
Comments |
||||||
From |
To |
Interval |
Au |
Ag |
Cu |
Pb |
Zn |
||
WGP-010 |
35 |
36 |
1 |
2.03 |
1.6 |
35 |
23 |
164 |
Vein #1 |
WGP-011 |
24 |
25 |
1 |
2.35 |
10.1 |
215 |
900 |
1,390 |
Vein #1 |
WGP-012 |
50 |
52 |
2 |
3.66 |
24.3 |
36 |
867 |
75 |
Vein #1 |
WGP-018 |
21 |
22 |
1 |
3.25 |
24.0 |
221 |
2,870 |
3,100 |
Vein #2 |
WGP-023 |
68 |
69 |
1 |
4.00 |
4.9 |
217 |
7 |
1,800 |
Vein #3 |
孔ID |
交叉點(M) |
化驗(Ppm) |
評論 |
||||||
從… |
至 |
間隔 |
Au |
銀 |
CU |
鉛 |
鋅 |
||
WGP-010 |
35歲 |
36 |
1 |
2.03 |
1.6 |
35歲 |
23個 |
一百六十四 |
1號靜脈 |
WGP-011 |
24個 |
25個 |
1 |
2.35 |
10.1 |
215 |
九百 |
1390 |
1號靜脈 |
WGP-012 |
50 |
52 |
2. |
3.66 |
24.3 |
36 |
八百六十七 |
75 |
1號靜脈 |
WGP-018 |
21歲 |
22 |
1 |
3.25 |
24.0 |
221 |
2870 |
3,100 |
2號脈 |
WGP-023 |
68 |
69 |
1 |
4.00 |
4.9 |
217 |
7. |
1800 |
3號脈 |
Table 4: Significant intersections from West Garida
表4:西加裡達的重要十字路口
The drill holes generally intersected the targeted mineralised structures (Veins #1, #2 and #3, see Figure 3). All mineralised intercepts from the West Garida drilling are provided in Appendix A, with significant intersections shown in Table 4 above. The drilling largely confirmed the presence and continuity of the shallow dipping mineralised structures, but did not replicate the high grades from surface sampling of the coarse-gold bearing structures, nor the results of hole WGP-003 (see news release dated September 1, 2022).
鑽孔一般與目標礦化構造(1號、2號和3號礦脈,見圖3)相交。West Garida鑽探的所有礦化截獲均載於附錄A,重要交叉點見上文表4。鑽探在很大程度上證實了淺層傾斜礦化構造的存在和連續性,但沒有複製粗含金構造地表採樣的高品位,也沒有複製WGP-003孔的結果(見日期為2022年9月1日的新聞稿)。
Abu Gaharish
阿布·加哈裡什
Hole ID |
Collar co-ordinates 1,2 |
EOH depth (m) |
Dip |
Grid azimuth |
Comments |
||
X |
Y |
Z |
|||||
GHP-001 |
564503.2 |
2917326.1 |
481.7 |
200 |
-53.1 |
79.6 |
Main Zone |
GHP-002 |
564431.0 |
2917336.0 |
477.3 |
200 |
-53.4 |
79.0 |
Main Zone |
GHP-003 |
564372.9 |
2917345.9 |
478.1 |
150 |
-52.0 |
90.9 |
Main Zone |
GHP-004 |
564307.4 |
2917342.2 |
478.8 |
150 |
-55.6 |
88.5 |
Main Zone |
GHP-005 |
564239.3 |
2917351.0 |
478.1 |
120 |
-56.5 |
93.0 |
Main Zone |
GHP-006 |
564488.8 |
2917177.5 |
480.7 |
200 |
-53.8 |
91.0 |
Main Zone |
GHP-007 |
564420.8 |
2917179.8 |
479.6 |
200 |
-55.0 |
90.3 |
Main Zone |
GHP-008 |
564347.1 |
2917185.3 |
483.0 |
150 |
-55.3 |
90.4 |
Main Zone |
GHP-009 |
564701.8 |
2916804.0 |
516.5 |
150 |
-54.1 |
90.3 |
SE shear |
GHP-010 |
564630.2 |
2916659.1 |
533.2 |
120 |
-54.8 |
88.2 |
SE shear |
GHP-011 |
564406.4 |
2916699.0 |
495.9 |
100 |
-53.7 |
89.4 |
SW shear |
GHP-012 |
563841.5 |
2916890.5 |
490.6 |
140 |
-49.7 |
70.9 |
Stockwork zone |
GHP-013 |
563919.9 |
2916955.1 |
508.9 |
140 |
-47.7 |
74.9 |
Stockwork zone |
GHP-014 |
563996.0 |
2916983.4 |
501.8 |
140 |
-50.8 |
71.5 |
Stockwork zone |
GHP-015 |
564566.5 |
2917491.7 |
470.6 |
150 |
-53.7 |
88.7 |
Main Zone |
GHP-016 |
564523.1 |
2917500.6 |
475.4 |
200 |
-53.4 |
84.3 |
Main Zone |
GHP-017 |
564447.2 |
2917507.1 |
474.2 |
160 |
-54.0 |
89.7 |
Main Zone |
GHP-018 |
564562.3 |
2918038.7 |
464.3 |
120 |
-54.5 |
89.9 |
Ionic leach anomaly |
GHP-019 |
564491.8 |
2918038.3 |
465.3 |
120 |
-55.0 |
90.9 |
Ionic leach anomaly |
GHP-020 |
564460.4 |
2918197.8 |
462.5 |
120 |
-53.1 |
90.7 |
Ionic leach anomaly |
GHP-021 |
564392.0 |
2918198.2 |
461.7 |
120 |
-54.7 |
91.4 |
Ionic leach anomaly |
GHP-022 |
564996.4 |
2918271.1 |
488.2 |
150 |
-54.9 |
105.3 |
NEX Vein zone |
Notes:
|
孔ID |
領座標系1,2 |
EOH深度(米) |
浸漬 |
柵格方位角 |
評論 |
||
X |
是的 |
Z |
|||||
GHP-001 |
564503.2 |
2917326.1 |
481.7 |
200個 |
-53.1 |
79.6 |
主區 |
GHP-002 |
564431.0 |
2917336.0 |
477.3 |
200個 |
-53.4 |
79.0 |
主區 |
GHP-003 |
564372.9 |
2917345.9 |
478.1 |
一百五十 |
-52.0 |
90.9 |
主區 |
GHP-004 |
564307.4 |
2917342.2 |
478.8 |
一百五十 |
-55.6 |
88.5 |
主區 |
GHP-005 |
564239.3 |
2917351.0 |
478.1 |
120 |
-56.5 |
93.0 |
主區 |
GHP-006 |
564488.8 |
2917177.5 |
480.7 |
200個 |
-53.8 |
91.0 |
主區 |
GHP-007 |
564420.8 |
2917179.8 |
479.6 |
200個 |
-55.0 |
90.3 |
主區 |
GHP-008 |
564347.1 |
2917185.3 |
483.0 |
一百五十 |
-55.3 |
90.4 |
主區 |
GHP-009 |
564701.8 |
2916804.0 |
516.5 |
一百五十 |
-54.1 |
90.3 |
Se切變 |
GHP-010 |
564630.2 |
2916659.1 |
533.2 |
120 |
-54.8 |
88.2 |
Se切變 |
GHP-011 |
564406.4 |
2916699.0 |
495.9 |
100個 |
-53.7 |
89.4 |
西南剪切力 |
GHP-012 |
563841.5 |
2916890.5 |
490.6 |
140 |
-49.7 |
70.9 |
網格區 |
GHP-013 |
563919.9 |
2916955.1 |
508.9 |
140 |
-47.7 |
74.9 |
網格區 |
GHP-014 |
563996.0 |
2916983.4 |
501.8 |
140 |
-50.8 |
71.5 |
網格區 |
GHP-015 |
564566.5 |
2917491.7 |
470.6 |
一百五十 |
-53.7 |
88.7 |
主區 |
GHP-016 |
564523.1 |
2917500.6 |
475.4 |
200個 |
-53.4 |
84.3 |
主區 |
GHP-017 |
564447.2 |
2917507.1 |
474.2 |
160 |
-54.0 |
89.7 |
主區 |
GHP-018 |
564562.3 |
2918038.7 |
464.3 |
120 |
-54.5 |
89.9 |
離子浸出異常 |
GHP-019 |
564491.8 |
2918038.3 |
465.3 |
120 |
-55.0 |
90.9 |
離子浸出異常 |
GHP-020 |
564460.4 |
2918197.8 |
462.5 |
120 |
-53.1 |
90.7 |
離子浸出異常 |
GHP-021 |
564392.0 |
2918198.2 |
461.7 |
120 |
-54.7 |
91.4 |
離子浸出異常 |
GHP-022 |
564996.4 |
2918271.1 |
488.2 |
一百五十 |
-54.9 |
105.3 |
NEX靜脈帶 |
備註:
|
Table 5: Collar details of RC exploration drill holes at Abu Gaharish
表5:阿布·加哈裡什的RC勘探鑽孔的接箍細節
22 drill holes, GHP-001 to GHP-022, were completed at the Abu Gaharish prospect (Figure 1), for a total of 3,300m metres (Table 5 and Figure 4) in this first pass programme. Holes were drilled over a broad area covering c. 1.7km of strike length of mineralisation that roughly parallels the contact of the Gaharish alkali granite pluton with the surrounding metasedimentary and metavolcanic package of country rocks. 11 holes were drilled at the Gaharish Main Zone, which was the main focus of ancient and recent artisanal mine workings (GHP-001 to GHP-008, and GHP-015 to GHP-017), 3 holes were drilled to test shear structures located within country rock package (GHP-009 to GHP-011), 3 holes were drilled to test a possible stockwork and sheeted vein zone southwest of the Main Zone, and within the Gaharish pluton itself (GHP-012 to GHP-014), 4 holes were drilled to test an ionic leach wadi sediment geochemical anomaly (GHP-018 to GHP-021), and the final hole was drilled to test the North East Extension ("NEX") Vein structure, along strike and north-northeast of the Main Zone (GHP-022). The collar locations of all the drill holes are shown in Figure 4.
在這一第一次通過方案中,在Abu Gaharish探區完成了22個鑽孔,從GHP-001到GHP-022(圖1),總長度為3,300米(表5和圖4)。在覆蓋範圍很廣的區域上鑽了幾個洞c.礦化走向長1.7公里,大致平行於加哈裡什鹼性花崗巖巖體與周圍的變質沉積和變質火山岩包圍巖的接觸。在加哈裡什主帶(GHP-001至GHP-008和GHP-015至GHP-017)上鑽了11個孔,以測試圍巖包內的剪切構造(GHP-009至GHP-011),鑽了3個孔以測試主帶西南可能存在的網狀和席狀脈帶,以及在加哈裡什巖體本身(GHP-012至GHP-014)內,鑽了4個孔以測試離子浸出瓦迪沉積物地球化學異常(GHP-018至GHP-021),最後一口井是為了測試沿著主帶走向和東北偏北方向(GHP-022)的東北延伸(NEX)礦脈結構。所有鑽孔的卡箍位置如圖4所示。
Figure 4: Abu Gaharish drill hole collar plan
圖4:阿布·加哈裡什鑽孔卡箍平面圖
All mineralised intercepts from the Abu Gaharish drilling are provided in Appendix B, with significant intersections shown in Table 6. The drilling identified a broad mineralised envelope over a c. 350m strike length associated with the Main Zone, containing higher grade structures, which returned intercepts including 2m @ 8.16 g/t Au and 3m @ 4.61 g/t Au. Screen fire assay of a single 1m sample indicated the presence of coarse gold in these zones. Narrow lower grade intercepts were returned from the southern shear structures in the country rocks, and a broad low grade interval in hole GHP-012 indicated the potential for sheeted vein style reduced intrusion-related gold ("RIRG") style mineralisation to the southwest of the Main Zone.
來自Abu Gaharish鑽探的所有礦化截獲物都在附錄B中提供,重要的交叉點如表6所示。鑽探發現了一個廣泛的礦化包層c.與主區有關的350米走向長度,包含較高品位的構造,返回的截距包括2M@8.16g/t Au和3m@4.61g/t Au。對一個1M樣品的螢幕火法分析表明,這些區域中存在粗金。圍巖中的南向剪切構造返回了較窄的低品位截距,GHP-012孔中較寬的低品位間隔表明,主帶西南部可能存在席狀脈型減少與侵入體相關的金礦(“RIRG”)型礦化。
Hole ID |
Intersection (m) |
Assays (ppm) |
Comments |
||||||
From |
To |
Interval |
Au |
Ag |
Cu |
Pb |
Zn |
||
GHP-001 |
1 |
5 |
4 |
2.70 |
2.2 |
69 |
193 |
181 |
Main Zone |
and |
61 |
70 |
9 |
2.10 |
2.3 |
57 |
385 |
457 |
|
incl. |
65 |
67 |
2 |
8.16 |
8.3 |
205 |
1,568 |
1,706 |
|
GHP-002 |
55 |
56 |
1 |
6.69 |
10.2 |
70 |
750 |
363 |
Main Zone |
GHP-006 |
80 |
83 |
3 |
3.27 |
5.9 |
47 |
199 |
394 |
Main Zone |
and |
124 |
126 |
2 |
3.52 |
8.1 |
58 |
126 |
359 |
|
GHP-007 |
8 |
10 |
2 |
3.78 |
1.3 |
14 |
190 |
188 |
Main Zone |
GHP-015 |
11 |
13 |
2 |
2.98 |
4.1 |
40 |
200 |
329 |
Main Zone |
and |
49 |
50 |
1 |
4.77 |
- |
- |
- |
- |
Gold by screen fire assay, coarse gold present |
GHP-016 |
37 |
42 |
5 |
1.23 |
0.5 |
14 |
26 |
102 |
Main Zone |
and |
49 |
52 |
3 |
4.61 |
14.8 |
186 |
967 |
849 |
孔ID |
交叉點(M) |
化驗(Ppm) |
評論 |
||||||
從… |
至 |
間隔 |
Au |
銀 |
CU |
鉛 |
鋅 |
||
GHP-001 |
1 |
5. |
4. |
2.70 |
2.2 |
69 |
一百九十三 |
181 |
主區 |
和 |
61 |
70 |
9 |
2.10 |
2.3 |
57 |
385 |
四百五十七 |
|
包括 |
65 |
67 |
2. |
8.16 |
8.3 |
205 |
1568 |
1706 |
|
GHP-002 |
55 |
56 |
1 |
6.69 |
10.2 |
70 |
750 |
363 |
主區 |
GHP-006 |
80 |
83 |
3. |
3.27 |
5.9 |
47 |
一百九十九 |
三九四 |
主區 |
和 |
124 |
126 |
2. |
3.52 |
8.1 |
58 |
126 |
359 |
|
GHP-007 |
8個個 |
10 |
2. |
3.78 |
1.3 |
14. |
190 |
188 |
主區 |
GHP-015 |
11. |
13個 |
2. |
2.98 |
4.1 |
40歲 |
200個 |
三百二十九 |
主區 |
和 |
49 |
50 |
1 |
4.77 |
- |
- |
- |
- |
螢幕火試金,粗金存在 |
GHP-016 |
37 |
42 |
5. |
1.23 |
0.5 |
14. |
26 |
一百零二 |
主區 |
和 |
49 |
52 |
3. |
4.61 |
14.8 |
一百八十六 |
967 |
849 |
Table 6: Significant intersections from Abu Gaharish
表6:阿布加哈裡什的重要十字路口
Sampling and analytical procedures
取樣和分析程式
The RC holes were drilled at 53⁄4" or 51⁄2" diameter, and the bulk percussion chip samples were collected directly into pre-written large plastic bags from the cyclone every metre, numbered with the hole number and hole depths, and laid out sequentially at the drill site. Between each metre of drilling the cyclone and top box were cleaned out with compressed air. The bags were logged on the drill sites by Aton geologists. The bulk 1m samples were weighed, and subsequently riffle split through a 3-tier splitter onsite by Aton field staff to produce an approximately 1/8 split, which was collected in cloth bags, numbered and tagged with the hole number and depth. The splitter was cleaned with compressed air between each sample. The reject material from this initial bulk split was re-bagged, labelled and tagged, and retained on the drill sites. A representative sample of each metre was washed and stored in marked plastic chip trays, each containing 20m of samples, photographed, and retained onsite as a permanent record of the drill hole.
RC孔的直徑為53⁄4“或51⁄2”,將塊狀沖擊切屑樣本每米直接從旋風分離器收集到預先寫入的大塑膠袋中,標有孔數和孔深,並在鑽探現場順序鋪設。在鑽井的每一米之間,旋風分離器和頂盒被壓縮空氣清理乾淨。這些袋子是由艾頓地質學家記錄在鑽探現場的。對散裝的100萬個樣品稱重,然後由Aton現場工作人員通過三層分離器進行Riffle裂解,產生大約1/8的裂解,收集在布袋中,編號並標記孔數和深度。在每個樣品之間用壓縮空氣清潔分離器。從最初的散裝裂解中產生的廢品被重新裝袋、貼上標籤和標籤,並保留在鑽探現場。每米的代表性樣本被清洗並儲存在標有標記的塑料晶片託盤中,每個託盤包含20米的樣本,拍照並保留在現場,作為鑽孔的永久記錄。
The 1m split samples, weighing approximately 5kg each were then transported to the Rodruin sample processing facility, where they were 1/2 riffle split into 2 separate sub-samples, weighing approximately 2.5kg. One of these sub-samples was marked and labelled, and retained at the laboratory for storage. The second 1m sub-samples were then combined into 4m composite samples, weighing approximately 10kg. These were thoroughly mixed and again riffle split to produce nominal c. 250-500g 4m composite samples which were dispatched to ALS Minerals for analysis. Again the splitter was cleaned with compressed air between each sample. The 4m composite samples were allocated new sample numbers. The bulk reject material from the riffle split 4m composite samples was disposed of. QAQC samples were inserted into the 4m composite sample stream at a rate of approximately 1 certified reference material (or "standard" sample) every 60 samples, 1 blank sample every 30 samples, and 1 field duplicate split sample every 30 samples.
然後,將100萬個分開的樣品,每個重約5千克,運輸到羅德魯魯樣品處理設施,在那裡它們被分成兩個單獨的子樣品,重約2.5千克。其中一個樣本被標記和貼上標籤,並保留在實驗室儲存。然後,將第二個100萬個子樣本組合成4M個重約10公斤的復合樣本。它們完全混合在一起,再一次混雜在一起,產生名義上的c.250-500克4M復合樣品,送至ALS Minerals進行分析。同樣,在每個樣品之間用壓縮空氣清潔分離器。這400萬個復合樣本被分配了新的樣本號。處理了4M複合材料試件的散裝廢品。將QAQC樣品以每60個樣品約1個認證標準物質(或“標準”樣品)、每30個樣品1個空白樣品、以及每30個樣品1個現場複製分離樣品的速率插入4M復合樣品流中。
The 4m composite samples were shipped to ALS Minerals sample preparation laboratory at Marsa Alam, Egypt, where they were pulverised to a size fraction of better than 85% passing 75 microns. From this pulverised material a further sub-sample was split off with a nominal c. 50g size, which was shipped on to ALS Minerals at Rosia Montana, Romania for analysis. The 4m composite samples were analysed for gold by fire assay with an atomic absorption spectroscopy ("AAS") finish (analytical code Au-AA23. Any high grade samples (Au >10 g/t) were re-analysed using analytical code Au-GRA21 (also fire assay, with a gravimetric finish).
這400萬個復合樣品被運往埃及Marsa Alam的ALS Minerals樣品製備實驗室,在那裡它們被粉碎成超過85%的粒度分數,超過75微米。從這種粉碎的材料中分離出另一個亞樣,標稱為c.50克大小,運往羅馬尼亞羅西亞·蒙大拿的ALS Minerals進行分析。用火焰原子吸收光譜儀(AAS)(分析代碼Au-aa23)分析了4M復合樣品中的金。任何高品位樣品(Au>10g/t)都用分析代碼Au-GRA21重新分析(也是火試,重量法)。
Upon receipt of the final 4m composite assay results from ALS, a number of the retained 1m sub-samples were selected by a senior Aton geologist for re-assaying, corresponding to 4m composite assays deemed to be of significance. The selected 1m sub-samples were again riffle split to produce nominal c. 250-500g 1m split samples which were again allocated new sample numbers. These were dispatched to ALS Minerals for the same sample preparation at Marsa Alam, and for subsequent analysis at Rosia Montana. The bulk reject material from the 1m sub-sample splits was re-bagged and retained onsite for storage at Rodruin. QAQC samples were inserted into the 1m split sample stream at a rate of approximately 1 standard every 30 samples, 1 blank sample every 15 samples, and 1 field duplicate split sample every 15 samples.
在收到ALS的最終4M復合化驗結果後,保留的1M個子樣本中的一些由高級Aton地質學家選擇重新進行化驗,與被認為有意義的4M個復合化驗相對應。選擇的100萬個子樣本再次進行抽籤分裂,以產生標稱c.250-500g 1M拆分樣本,再次分配新的樣本號。這些樣品被送往ALS Minerals,在Marsa Alam進行同樣的樣品製備,並在Rosia Montana進行後續分析。從100萬個子樣分離出來的大塊廢品被重新打包,並保留在現場儲存在羅德魯魯。QAQC樣本以大約每30個樣本1個標準、每15個樣本1個空白樣本、以及每15個樣本1個現場複製分裂樣本的速率插入到1M分裂樣本流中。
The 1m split samples were again analysed for gold by fire assay (analytical code Au-AA23), and for silver, copper, lead and zinc using an aqua regia digest followed by an AAS finish (analytical code AA45). Any high grade gold samples (Au >10 g/t) were again re-analysed using analytical code Au-GRA21 (also fire assay, with a gravimetric finish). Any high grade Ag and base metal samples (Ag >100 g/t, and Cu, Pb and Zn >10,000ppm or >1%) were re-analysed using the ore grade technique AA46 (also an aqua regia digest followed by an AAS finish).
用火分析法(分析代碼Au-aa23)再次分析了這100萬個分開的樣品中的金,並使用王水消化和原子吸收光譜分析(分析代碼AA45)分析了銀、銅、鉛和鋅。任何高品位黃金樣品(Au>10g/t)再次使用分析代碼Au-GRA21(也是火試金,重量法)進行重新分析。任何高品位的銀和賤金屬樣品(銀>100克/噸,銅、鉛和鋅>10,000ppm或>1%)都用礦石品位技術AA46(也是王水消化和原子吸收光譜分析)重新分析。
All intersections herein reported relate to 1m split samples.
本文報告的所有交叉點都涉及100萬個分離樣本。
About Aton Resources Inc. Aton Resources Inc. (AAN: TSX-V) is focused on its 100% owned Abu Marawat Concession ("Abu Marawat"), located in Egypt's Arabian-Nubian Shield, approximately 200 km north of Centamin's world-class Sukari gold mine. Aton has identified numerous gold and base metal exploration targets at Abu Marawat, including the Hamama deposit in the west, the Abu Marawat deposit in the northeast, and the advanced Rodruin exploration prospect in the south of the Concession. Two historic British gold mines are also located on the Concession at Sir Bakis and Semna. Aton has identified several distinct geological trends within Abu Marawat, which display potential for the development of a variety of styles of precious and base metal mineralisation. Abu Marawat is 447.7 km 2 in size and is located in an area of excellent infrastructure; a four-lane highway, a 220kV power line, and a water pipeline are in close proximity, as are the international airports at Hurghada and Luxor. |
Qualified person The technical information contained in this News Release was prepared by Javier Orduña BSc (hons), MSc, MCSM, DIC, MAIG, SEG(M), Exploration Manager of Aton Resources Inc. Mr. Orduña is a qualified person (QP) under National Instrument 43-101 Standards of Disclosure for Mineral Projects. |
Some of the statements contained in this release are forward-looking statements. Since forward-looking statements address future events and conditions; by their very nature they involve inherent risks and uncertainties. Actual results in each case could differ materially from those currently anticipated in such statements. |
關於艾頓資源公司 Aton Resources Inc.(AAN:TSX-V)專注於其100%擁有的Abu Marawat特許權(“Abu Marawat”),該特許權位於埃及的阿拉伯-努比亞盾牌,位於Centamin世界級Sukari金礦以北約200公里處。Aton已在Abu Marawat確定了許多金礦和賤金屬勘探目標,包括西部的Hamama礦床、東北部的Abu Marawat礦床以及特許權南部的高級Rodruum勘探前景。兩座歷史悠久的英國金礦也位於巴基斯爵士和塞姆納的特許權上。Aton已在Abu Marawat確定了幾個不同的地質趨勢,這些趨勢顯示出開發各種類型的貴金屬和賤金屬礦化的潛力。阿布馬拉瓦特距離447.7公里2.酒店佔地面積大,地處基礎設施完善的地區;附近有一條四車道駭維金屬加工、一條220千伏輸電線和一條輸水管道,赫爾加達和盧克索的國際機場也是如此。 |
有資格的人 本新聞稿中包含的技術資訊由Aton Resources Inc.勘探經理Javier Orduña BSC(榮譽),MSC,MCSM,DIC,MAIG,SEG(M)編寫。Orduña先生是National Instrument 43-101礦產專案披露標準下的合格人員(QP)。 |
本新聞稿中包含的一些陳述是前瞻性陳述。由於前瞻性陳述涉及未來的事件和情況,因此它們本身就涉及固有的風險和不確定因素。每一種情況的實際結果都可能與此類陳述中目前預期的結果大不相同。 |
Appendix A - Significant intersections from the West Garida prospect
附錄A-西加裡達前景的重要交叉口
Hole ID |
Intersection (m) |
Assays (ppm) |
Comments |
||||||
From |
To |
Interval |
Au |
Ag |
Cu |
Pb |
Zn |
||
WGP-006 |
67 |
68 |
1 |
0.34 |
1.3 |
68 |
11 |
230 |
|
WGP-007 |
85 |
86 |
1 |
0.42 |
2.0 |
91 |
16 |
248 |
|
WGP-008a |
86 |
87 |
1 |
0.42 |
3.6 |
71 |
25 |
875 |
|
WGP-009 |
72 |
75 |
3 |
0.68 |
2.4 |
151 |
24 |
2,821 |
|
WGP-010 |
28 |
29 |
1 |
1.37 |
1.2 |
84 |
155 |
875 |
|
and |
35 |
36 |
1 |
2.03 |
1.6 |
35 |
23 |
164 |
|
WGP-011 |
24 |
25 |
1 |
2.35 |
10.1 |
215 |
900 |
1,390 |
|
WGP-012 |
50 |
52 |
2 |
3.66 |
24.3 |
36 |
867 |
75 |
|
WGP-013 |
- |
- |
- |
- |
- |
- |
- |
- |
NSA > 0.06 g/t Au |
WGP-014 |
- |
- |
- |
- |
- |
- |
- |
- |
NSA > 0.04 g/t Au |
WGP-015 |
- |
- |
- |
- |
- |
- |
- |
- |
NSA > 0.17 g/t Au |
WGP-016 |
- |
- |
- |
- |
- |
- |
- |
- |
NSA > 0.20 g/t Au |
WGP-017 |
23 |
25 |
2 |
1.79 |
33.2 |
509 |
497 |
3,595 |
|
WGP-018 |
21 |
22 |
1 |
3.25 |
24.0 |
221 |
2,870 |
3,100 |
|
WGP-019 |
25 |
26 |
1 |
1.90 |
18.6 |
106 |
1,445 |
1,360 |
|
WGP-020 |
- |
- |
- |
- |
- |
- |
- |
- |
NSA > 0.04 g/t Au |
WGP-021 |
32 |
34 |
2 |
0.32 |
1.1 |
156 |
35 |
2,240 |
|
WGP-022 |
21 |
22 |
1 |
0.40 |
0.3 |
45 |
8 |
299 |
|
and |
33 |
34 |
1 |
0.36 |
0.8 |
54 |
13 |
177 |
|
and |
51 |
52 |
1 |
0.47 |
0.5 |
74 |
10 |
76 |
|
WGP-023 |
49 |
50 |
1 |
0.62 |
1.3 |
71 |
11 |
720 |
|
and |
68 |
69 |
1 |
4.00 |
4.9 |
217 |
7 |
1,800 |
|
WGP-024 |
20 |
22 |
2 |
0.70 |
15.7 |
527 |
847 |
1,870 |
|
WGP-025 |
26 |
27 |
1 |
0.55 |
24.0 |
242 |
819 |
1,705 |
|
Notes:
|
孔ID |
交叉點(M) |
化驗(Ppm) |
評論 |
||||||
從… |
至 |
間隔 |
Au |
銀 |
CU |
鉛 |
鋅 |
||
WGP-006 |
67 |
68 |
1 |
0.34 |
1.3 |
68 |
11. |
230 |
|
WGP-007 |
85 |
86 |
1 |
0.42 |
2.0 |
91 |
16年 |
248 |
|
WGP-008a |
86 |
八十七 |
1 |
0.42 |
3.6 |
71 |
25個 |
八百七十五 |
|
WGP-009 |
72 |
75 |
3. |
0.68 |
2.4 |
151 |
24個 |
2821 |
|
WGP-010 |
28 |
29 |
1 |
1.37 |
1.2 |
84 |
一百五十五 |
八百七十五 |
|
和 |
35歲 |
36 |
1 |
2.03 |
1.6 |
35歲 |
23個 |
一百六十四 |
|
WGP-011 |
24個 |
25個 |
1 |
2.35 |
10.1 |
215 |
九百 |
1390 |
|
WGP-012 |
50 |
52 |
2. |
3.66 |
24.3 |
36 |
八百六十七 |
75 |
|
WGP-013 |
- |
- |
- |
- |
- |
- |
- |
- |
國家安全局>0.06克/噸Au |
WGP-014 |
- |
- |
- |
- |
- |
- |
- |
- |
國家安全局>0.04克/噸Au |
WGP-015 |
- |
- |
- |
- |
- |
- |
- |
- |
國家安全局>0.17克/噸Au |
WGP-016 |
- |
- |
- |
- |
- |
- |
- |
- |
國家安全局>0.20克/噸Au |
WGP-017 |
23個 |
25個 |
2. |
1.79 |
33.2 |
五百零九 |
497 |
3595 |
|
WGP-018 |
21歲 |
22 |
1 |
3.25 |
24.0 |
221 |
2870 |
3,100 |
|
WGP-019 |
25個 |
26 |
1 |
1.90 |
18.6 |
106 |
1445 |
1360 |
|
WGP-020 |
- |
- |
- |
- |
- |
- |
- |
- |
國家安全局>0.04克/噸Au |
WGP-021 |
32位 |
34 |
2. |
0.32 |
1.1 |
一百五十六 |
35歲 |
2240 |
|
WGP-022 |
21歲 |
22 |
1 |
0.40 |
0.3 |
45 |
8個個 |
299 |
|
和 |
33 |
34 |
1 |
0.36 |
0.8 |
54 |
13個 |
177 |
|
和 |
51 |
52 |
1 |
0.47 |
0.5 |
74 |
10 |
76 |
|
WGP-023 |
49 |
50 |
1 |
0.62 |
1.3 |
71 |
11. |
720 |
|
和 |
68 |
69 |
1 |
4.00 |
4.9 |
217 |
7. |
1800 |
|
WGP-024 |
20個 |
22 |
2. |
0.70 |
15.7 |
527 |
八四七 |
1870 |
|
WGP-025 |
26 |
27 |
1 |
0.55 |
24.0 |
242 |
819 |
1,705 |
|
備註:
|
Appendix B - Significant intersections from the Abu Gaharish prospect
附錄B-阿布加哈裡什地區的重要交叉路口
Hole ID |
Intersection (m) |
Assays (ppm) |
Comments |
||||||
From |
To |
Interval |
Au |
Ag |
Cu |
Pb |
Zn |
||
GHP-001 |
1 |
5 |
4 |
2.70 |
2.2 |
69 |
193 |
181 |
Main Zone |
and |
18 |
19 |
1 |
2.82 |
5.1 |
31 |
733 |
344 |
|
and |
51 |
53 |
2 |
1.38 |
1.4 |
17 |
93 |
215 |
|
and |
61 |
70 |
9 |
2.10 |
2.3 |
57 |
385 |
457 |
|
incl. |
65 |
67 |
2 |
8.16 |
8.3 |
205 |
1,568 |
1,706 |
|
and |
76 |
77 |
1 |
3.19 |
2.2 |
12 |
315 |
1010 |
|
and |
96 |
97 |
1 |
0.88 |
5.1 |
17 |
223 |
349 |
|
GHP-002 |
55 |
56 |
1 |
6.69 |
10.2 |
70 |
750 |
363 |
Main Zone |
and |
98 |
100 |
2 |
0.79 |
1.2 |
22 |
38 |
48 |
|
and |
115 |
116 |
1 |
0.51 |
1.2 |
11 |
35 |
58 |
|
GHP-003 |
96 |
97 |
1 |
0.50 |
0.9 |
48 |
10 |
65 |
Main Zone |
GHP-004 |
87 |
88 |
1 |
0.63 |
0.7 |
28 |
8 |
53 |
Main Zone |
GHP-005 |
12 |
13 |
1 |
1.03 |
0.8 |
17 |
85 |
32 |
Main Zone |
GHP-006 |
68 |
69 |
1 |
0.58 |
0.8 |
14 |
27 |
83 |
Main Zone |
and |
80 |
83 |
3 |
3.27 |
5.9 |
47 |
199 |
394 |
|
and |
124 |
126 |
2 |
3.52 |
8.1 |
58 |
126 |
359 |
|
and |
131 |
132 |
1 |
0.96 |
0.9 |
12 |
89 |
346 |
|
GHP-007 |
8 |
10 |
2 |
3.78 |
1.3 |
14 |
190 |
188 |
Main Zone |
and |
54 |
55 |
1 |
0.89 |
2.3 |
81 |
148 |
125 |
|
and |
67 |
68 |
1 |
0.73 |
1.2 |
19 |
9 |
82 |
|
and |
112 |
113 |
1 |
0.50 |
0.7 |
15 |
21 |
59 |
|
GHP-008 |
59 |
60 |
1 |
1.13 |
0.5 |
14 |
22 |
58 |
Main Zone |
and |
102 |
104 |
2 |
0.79 |
0.8 |
6 |
11 |
58 |
|
and |
141 |
142 |
1 |
0.50 |
2.0 |
13 |
60 |
138 |
|
GHP-009 |
- |
- |
- |
- |
- |
- |
- |
- |
NSA > 0.265 g/t Au (SE Shear) |
GHP-010 |
43 |
44 |
1 |
0.64 |
1.2 |
58 |
8 |
82 |
SE Shear |
GHP-011 |
55 |
57 |
2 |
1.36 |
0.9 |
35 |
27 |
111 |
SW Shear |
GHP-012 3 |
0 |
29 |
29 |
0.28 |
0.3 |
9 |
15 |
56 |
Stockwork zone, possible RIRG style mineralisation? |
GHP-013 |
52 |
53 |
1 |
2.50 |
3.4 |
8 |
29 |
79 |
Stockwork zone |
and |
75 |
78 |
3 |
0.51 |
0.6 |
8 |
25 |
76 |
|
GHP-014 |
- |
- |
- |
- |
- |
- |
- |
- |
NSA > 0.213 g/t Au (stockwork zone) |
GHP-015 |
11 |
13 |
2 |
2.98 |
4.1 |
40 |
200 |
329 |
Main Zone |
and |
17 |
19 |
2 |
0.89 |
1.9 |
17 |
63 |
136 |
|
and |
34 |
35 |
1 |
1.02 |
1.1 |
21 |
77 |
208 |
|
and |
49 |
50 |
1 |
4.77 |
- |
- |
- |
- |
Gold by screen fire assay, coarse gold present |
and |
55 |
57 |
2 |
1.60 |
1.3 |
21 |
60 |
221 |
|
GHP-016 |
12 |
13 |
1 |
0.57 |
0.6 |
12 |
106 |
131 |
Main Zone |
and |
32 |
33 |
1 |
0.73 |
0.8 |
13 |
203 |
248 |
|
and |
37 |
42 |
5 |
1.23 |
0.5 |
14 |
26 |
102 |
|
and |
49 |
52 |
3 |
4.61 |
14.8 |
186 |
967 |
849 |
|
and |
61 |
62 |
1 |
1.46 |
1.4 |
6 |
80 |
198 |
|
Hole ID |
Intersection (m) |
Assays (ppm) |
Comments |
||||||
From |
To |
From |
To |
From |
To |
From |
To |
||
GHP-016 |
86 |
87 |
1 |
0.70 |
0.6 |
5 |
119 |
66 |
|
and |
90 |
91 |
1 |
0.72 |
1.2 |
11 |
59 |
87 |
|
and |
102 |
103 |
1 |
0.82 |
0.6 |
58 |
11 |
59 |
|
GHP-017 |
105 |
106 |
1 |
1.71 |
2.2 |
17 |
68 |
86 |
Main Zone |
and |
119 |
120 |
1 |
1.35 |
0.6 |
3 |
90 |
324 |
|
and |
123 |
125 |
2 |
0.65 |
0.9 |
15 |
30 |
66 |
|
GHP-018 |
- |
- |
- |
- |
- |
- |
- |
- |
NSA > 0.099 g/t Au (IL anomaly) |
GHP-019 |
- |
- |
- |
- |
- |
- |
- |
- |
NSA > 0.117 g/t Au (IL anomaly) |
GHP-020 |
- |
- |
- |
- |
- |
- |
- |
- |
NSA > 0.175 g/t Au (IL anomaly) |
GHP-021 |
- |
- |
- |
- |
- |
- |
- |
- |
NSA > 0.144 g/t Au (IL anomaly) |
GHP-022 |
- |
- |
- |
- |
- |
- |
- |
- |
NSA > 0.109 g/t Au (NEX Vein) |
Notes:
|
孔ID |
交叉點(M) |
化驗(Ppm) |
評論 |
||||||
從… |
至 |
間隔 |
Au |
銀 |
CU |
鉛 |
鋅 |
||
GHP-001 |
1 |
5. |
4. |
2.70 |
2.2 |
69 |
一百九十三 |
181 |
主區 |
和 |
18 |
19個 |
1 |
2.82 |
5.1 |
31 |
七百三十三 |
三百四十四 |
|
和 |
51 |
53 |
2. |
1.38 |
1.4 |
17 |
93 |
215 |
|
和 |
61 |
70 |
9 |
2.10 |
2.3 |
57 |
385 |
四百五十七 |
|
包括 |
65 |
67 |
2. |
8.16 |
8.3 |
205 |
1568 |
1706 |
|
和 |
76 |
77 |
1 |
3.19 |
2.2 |
12 |
315 |
1010 |
|
和 |
96 |
九十七 |
1 |
0.88 |
5.1 |
17 |
223 |
三百四十九 |
|
GHP-002 |
55 |
56 |
1 |
6.69 |
10.2 |
70 |
750 |
363 |
主區 |
和 |
98 |
100個 |
2. |
0.79 |
1.2 |
22 |
38 |
48 |
|
和 |
一百一十五 |
116 |
1 |
0.51 |
1.2 |
11. |
35歲 |
58 |
|
GHP-003 |
96 |
九十七 |
1 |
0.50 |
0.9 |
48 |
10 |
65 |
主區 |
GHP-004 |
八十七 |
88 |
1 |
0.63 |
0.7 |
28 |
8個個 |
53 |
主區 |
GHP-005 |
12 |
13個 |
1 |
1.03 |
0.8 |
17 |
85 |
32位 |
主區 |
GHP-006 |
68 |
69 |
1 |
0.58 |
0.8 |
14. |
27 |
83 |
主區 |
和 |
80 |
83 |
3. |
3.27 |
5.9 |
47 |
一百九十九 |
三九四 |
|
和 |
124 |
126 |
2. |
3.52 |
8.1 |
58 |
126 |
359 |
|
和 |
131 |
132 |
1 |
0.96 |
0.9 |
12 |
八十九 |
三百四十六 |
|
GHP-007 |
8個個 |
10 |
2. |
3.78 |
1.3 |
14. |
190 |
188 |
主區 |
和 |
54 |
55 |
1 |
0.89 |
2.3 |
八十一 |
148 |
125 |
|
和 |
67 |
68 |
1 |
0.73 |
1.2 |
19個 |
9 |
八十二 |
|
和 |
一百一十二 |
113 |
1 |
0.50 |
0.7 |
15個 |
21歲 |
59 |
|
GHP-008 |
59 |
60 |
1 |
1.13 |
0.5 |
14. |
22 |
58 |
主區 |
和 |
一百零二 |
104 |
2. |
0.79 |
0.8 |
6. |
11. |
58 |
|
和 |
一百四十一 |
一百四十二 |
1 |
0.50 |
2.0 |
13個 |
60 |
一百三十八 |
|
GHP-009 |
- |
- |
- |
- |
- |
- |
- |
- |
國家安全局>0.265克/噸Au(東南切變) |
GHP-010 |
43 |
44 |
1 |
0.64 |
1.2 |
58 |
8個個 |
八十二 |
東南向切變 |
GHP-011 |
55 |
57 |
2. |
1.36 |
0.9 |
35歲 |
27 |
111 |
西南切變 |
GHP-0123. |
0 |
29 |
29 |
0.28 |
0.3 |
9 |
15個 |
56 |
網狀區,可能是RIRG風格的礦化? |
GHP-013 |
52 |
53 |
1 |
2.50 |
3.4 |
8個個 |
29 |
79 |
網格區 |
和 |
75 |
78 |
3. |
0.51 |
0.6 |
8個個 |
25個 |
76 |
|
GHP-014 |
- |
- |
- |
- |
- |
- |
- |
- |
美國國家安全局>0.213克/噸Au(網眼區域) |
GHP-015 |
11. |
13個 |
2. |
2.98 |
4.1 |
40歲 |
200個 |
三百二十九 |
主區 |
和 |
17 |
19個 |
2. |
0.89 |
1.9 |
17 |
63 |
136 |
|
和 |
34 |
35歲 |
1 |
1.02 |
1.1 |
21歲 |
77 |
208 |
|
和 |
49 |
50 |
1 |
4.77 |
- |
- |
- |
- |
螢幕火試金,粗金存在 |
和 |
55 |
57 |
2. |
1.60 |
1.3 |
21歲 |
60 |
221 |
|
GHP-016 |
12 |
13個 |
1 |
0.57 |
0.6 |
12 |
106 |
131 |
主區 |
和 |
32位 |
33 |
1 |
0.73 |
0.8 |
13個 |
203 |
248 |
|
和 |
37 |
42 |
5. |
1.23 |
0.5 |
14. |
26 |
一百零二 |
|
和 |
49 |
52 |
3. |
4.61 |
14.8 |
一百八十六 |
967 |
849 |
|
和 |
61 |
62 |
1 |
1.46 |
1.4 |
6. |
80 |
一百九十八 |
|
孔ID |
交叉點(M) |
化驗(Ppm) |
評論 |
||||||
從… |
至 |
從… |
至 |
從… |
至 |
從… |
至 |
||
GHP-016 |
86 |
八十七 |
1 |
0.70 |
0.6 |
5. |
119 |
66 |
|
和 |
90 |
91 |
1 |
0.72 |
1.2 |
11. |
59 |
八十七 |
|
和 |
一百零二 |
103 |
1 |
0.82 |
0.6 |
58 |
11. |
59 |
|
GHP-017 |
一百零五 |
106 |
1 |
1.71 |
2.2 |
17 |
68 |
86 |
主區 |
和 |
119 |
120 |
1 |
1.35 |
0.6 |
3. |
90 |
324 |
|
和 |
123 |
125 |
2. |
0.65 |
0.9 |
15個 |
30個 |
66 |
|
GHP-018 |
- |
- |
- |
- |
- |
- |
- |
- |
美國國家安全局>0.099克/噸Au(IL異常) |
GHP-019 |
- |
- |
- |
- |
- |
- |
- |
- |
美國國家安全局>0.117克/噸Au(IL異常) |
GHP-020 |
- |
- |
- |
- |
- |
- |
- |
- |
美國國家安全局>0.175克/噸Au(IL異常) |
GHP-021 |
- |
- |
- |
- |
- |
- |
- |
- |
美國國家安全局>0.144克/噸Au(IL異常) |
GHP-022 |
- |
- |
- |
- |
- |
- |
- |
- |
NSA>0.109克/噸Au(NEX靜脈) |
備註:
|
SOURCE: Aton Resources, Inc.
資料來源:艾頓資源公司