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).
不列颠哥伦比亚省温哥华/ACCESSWIRE/2023年10月11日/Aton Resources Inc.(多伦多证券交易所股票代码:AAN)(以下简称“Aton”或“公司”)欣然宣布,在其全资拥有的位于埃及东部沙漠的Abu Marawat特许权(“Abu Marawat”或“特许权”),以及West Garida和Abu Gaharish矿区的第一批勘探结果(图1),已经完成了反循环冲击波(RC)项目钻探。
Highlights:
重点:
- 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勘探区块的区域勘探RC方案期间,共钻了85个孔,总长达11700米;
- 在Hamama项目区以西约20公里处的3个地下水勘探孔中又钻了628米;
- 从努比亚砂岩覆盖岩内的地下水勘探孔记录到大量流量,证明了该装置可以为计划中的Hamama West和Rodruum采矿项目提供工艺用水的概念;
- Abu Gaharish探矿的重要矿化交汇处包括9米@2.10克/吨金、3米@4.61克/吨金和3米@3.27克/吨金。金矿化主要集中在加哈里什主带的宽广矿化包体中;
- 西加里达狭窄的矿化交叉点包括来自1号矿脉的2m@3.66 g/t Au和24.3 g/t Ag,以及来自3号矿脉的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."
我们很高兴地宣布,区域资源中心在阿布马拉瓦特的勘探钻探计划已成功完成,并提供了第一批结果。临时首席执行官托诺·瓦克说。“我们对哈马以西努比亚砂岩的地下水钻探结果特别满意,该钻探旨在测试这些岩石的潜力,为计划在哈马西启动的堆浸采矿项目提供工艺水供应。钻探与努比亚盖层的大量地下水相交,取得了非常令人鼓舞的结果。特别令人鼓舞的是,钻探没有深入到与主要目标努比亚的塔里夫砂岩单元相交的深度,这表明该单元可能拥有大量地下水资源,比先前预期的更接近哈马岛。Emra根据Abu Marawat特许权协议的条款,继续审查我们提交给他们的详细介绍在Hamama West和Rodruum矿藏的商业发现的文件,我们希望这一进程正在朝着成功完成和颁发Abu Marawat采矿许可证的方向迈进。自2005年Sukari以来,埃及向公开上市的外国投资者发放的第一个黄金开采许可证将标志着Aton以及埃及、石油部和EMRA向前迈出了非常重要的一步。
2023 Abu Marawat RC drilling programme
2023年阿布马拉瓦特RC钻井方案
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钻探由GeoDrill的埃及分公司GeoDrill for Leating and Specialized Services Free Zone LLC进行,从Hamama West以东3公里处的West Garida勘探区块开始。在将钻井平台调动到Abu Gaharish之前,还钻了3个地下水勘探孔,以测试Hamama项目以西约20公里处的努比亚砂岩含水层。在Abu Gaharish的钻探,以及随后在Semna和Zeno的钻探都得到了苍蝇营地的支持。该方案的钻探米汇总在表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 |
项目 |
孔数 |
总米 |
地下水勘探(努比亚砂岩) |
3. |
六百二十八 |
西加里达 |
21岁 |
1,522 |
阿布·加哈里什 |
22 |
3300 |
塞姆纳 |
21岁 |
3662 |
泽诺 |
21岁 |
3216 |
总计 |
88 |
12,328 |
Table 1: Breakdown of the RC drilling completed
表1:RC钻探已完成的细目
Figure 1: Geology and prospect plan of the Abu Marawat Concession
图1:阿布马拉瓦特特许权的地质和远景规划
Groundwater exploration drilling
地下水勘探钻探
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矿藏以西约20公里处Hamama通道以南约20公里处钻探了2个HAW-01和HAW-02孔,以测试Nubian砂岩地层的潜力,为拟建的Hamama West生产足够数量的工艺水。HAW-03井是在HAW-01以东约4公里处向Hamama方向钻探的。孔的详细信息和位置见表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 |
领座标系1,2 |
EOH深度(米) |
浸渍 |
栅格方位角 |
评论 |
||
X |
是的 |
Z |
|||||
HAW-01 |
517072 |
2910962 |
二百九十一 |
100个 |
-90 |
- |
井眼干燥 |
HAW-02 |
516679 |
2909410 |
二百八十五 |
二百九十四 |
-90 |
- |
c.700 L/分钟水深270米 |
How-03 |
520792 |
2911753 |
315 |
二百三十四 |
-90 |
- |
c.480 L/分钟222m水深流量 |
备注:
|
Table 2: Collar details of groundwater exploration drill holes
表2:地下水勘探钻孔的卡箍细部
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孔的钻孔直径为53⁄4“,其中HAW-02和HAW-03孔的直径减少到51⁄2”。HAW-01和HAW-02孔穿过表层冲积席状沉积物至12m处,HAW-03孔至30m处。
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孔在其目标深度100米处未能与任何水相交,因此被终止。HAW-02和HAW-03两个孔都从大约120米深的地方与大量地下水相交,钻探人员无法保持孔和样品的干燥(图2)。由于HAW-02井在含水砂岩中坍塌,HAW-02井在294m处终止,HAW-03井在234米处终止。
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.
所有的孔都钻过了以棕色、红色、灰色和黑色为主的页岩和泥岩的杂色序列,夹层砂岩单元被解释为属于白垩纪努比亚砂岩建造的Quseir单元。努比亚砂岩组的目标塔里夫砂岩单元没有在三个孔中的任何一个相交。
Figure 2: Drilling on groundwater exploration hole HAW-02
图2:HAW-02地下水探测孔的钻探
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-03两个孔从大约120米开始产生大量的水,体积随着深度的增加而增加。水主要赋存于以页岩和泥岩为主的层序夹层的砂岩层内。使用增压压缩机在两个孔上进行了气升测试,但没有进行正式的泵测试。水流测量采用V型槽堰系统。从HAW-02和HAW-03两个孔记录到大量的水流,最大流量为c.在270m深度和220m深度分别为700 L/分钟和480 L/分钟。
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.
该方案成功地证明了这样一个概念,即Hamama地区以西露头的努比亚砂岩覆盖层可能拥有足够的地下水资源,为拟议的Hamama West露天矿山和堆浸项目提供工艺水。据指出,钻探未能与努比亚砂岩地层更深的塔里夫砂岩单元相交,该砂岩单元是该方案的主要目标。努比亚砂岩覆盖层向西向尼罗河流域倾斜,这表明塔里夫组含水层有可能交叉开采较浅深度的地下水,并进一步向东向Hamama项目开采,从而缩短了所需的抽水距离。
Exploration RC drilling
勘探RC钻探
West Garida
西加里达
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个钻孔在西加里达探矿完成(图1),总长度为1,522米(表3和图3)。West Garida的矿化与几个狭窄的浅层粗含金石英脉有关,钻探旨在跟进之前在WGP-003孔1米间隔内RC钻探交汇处的41.7克/吨金、263克/吨银和2.08%铅(见日期为2022年9月1日的新闻稿)。
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 |
领座标系1,2 |
EOH深度(米) |
浸渍 |
栅格方位角 |
评论 |
||
X |
是的 |
Z |
|||||
WGP-006 |
537327.4 |
2914773.9 |
630.6 |
100个 |
-71.3 |
0.8 |
1号静脉 |
WGP-007 |
537327.4 |
2914776.0 |
630.6 |
100个 |
-51.3 |
3.1 |
1号静脉 |
WGP-008 |
537327.1 |
2914762.7 |
630.6 |
57 |
-65.0 |
179.6 |
1号脉(已废弃的洞) |
WGP-008a |
537327.4 |
2914766.2 |
630.6 |
120 |
-64.8 |
181.1 |
1号脉(重钻WGP-008) |
WGP-009 |
537327.5 |
2914767.1 |
630.7 |
110 |
-78.7 |
180.6 |
1号静脉 |
WGP-010 |
537240.4 |
2914803.6 |
614.7 |
60 |
-48.1 |
1.4 |
1号静脉 |
WGP-011 |
537240.2 |
2914800.3 |
614.9 |
60 |
-89.5 |
351.9 |
1号静脉 |
WGP-012 |
537238.9 |
2914737.2 |
629.7 |
100个 |
-55.0 |
358.1 |
1号静脉 |
WGP-013 |
537239.0 |
2914735.6 |
629.8 |
100个 |
-74.3 |
1.1 |
1号静脉 |
WGP-014 |
537239.0 |
2914734.6 |
629.9 |
100个 |
-90.0 |
0.0 |
1号静脉 |
WGP-015 |
537239.1 |
2914728.3 |
630.1 |
110 |
-80.6 |
189.1 |
1号静脉 |
WGP-016 |
536845.5 |
2914990.0 |
637.6 |
40岁 |
-89.8 |
221.4 |
2号脉 |
WGP-017 |
536847.7 |
2914991.3 |
637.7 |
40岁 |
-50.0 |
59.5 |
2号脉 |
WGP-018 |
536797.7 |
2914961.8 |
634.3 |
40岁 |
-50.6 |
58.8 |
2号脉 |
WGP-019 |
536795.2 |
2914960.6 |
634.2 |
50 |
-89.6 |
335.8 |
2号脉 |
WGP-020 |
536790.9 |
2914958.3 |
633.9 |
75 |
-55.4 |
237.7 |
2号脉 |
WGP-021 |
536780.6 |
2915143.5 |
627.5 |
50 |
-50.5 |
129.2 |
3号脉 |
WGP-022 |
536778.6 |
2915145.1 |
627.4 |
60 |
-89.4 |
147.9 |
3号脉 |
WGP-023 |
536775.8 |
2915147.1 |
627.3 |
70 |
-59.2 |
311.5 |
3号脉 |
WGP-024 |
536836.9 |
2914991.5 |
637.2 |
40岁 |
-50.3 |
315.4 |
2号脉 |
WGP-025 |
536845.1 |
2914986.0 |
637.6 |
40岁 |
-50.1 |
179.5 |
2号脉 |
备注:
|
Table 3: Collar details of RC exploration drill holes at West Garida
表3:西加里达RC勘探钻孔的钻柱细节
Figure 3: West Garida drill hole collar plan
图3:西加里达钻孔卡箍平面图
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 |
交叉点(M) |
化验(Ppm) |
评论 |
||||||
从… |
至 |
间隔 |
Au |
银 |
CU |
铅 |
锌 |
||
WGP-010 |
35岁 |
36 |
1 |
2.03 |
1.6 |
35岁 |
23个 |
一百六十四 |
1号静脉 |
WGP-011 |
24个 |
25个 |
1 |
2.35 |
10.1 |
215 |
九百 |
1390 |
1号静脉 |
WGP-012 |
50 |
52 |
2. |
3.66 |
24.3 |
36 |
八百六十七 |
75 |
1号静脉 |
WGP-018 |
21岁 |
22 |
1 |
3.25 |
24.0 |
221 |
2870 |
3,100 |
2号脉 |
WGP-023 |
68 |
69 |
1 |
4.00 |
4.9 |
217 |
7. |
1800 |
3号脉 |
Table 4: Significant intersections from West Garida
表4:西加里达的重要十字路口
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).
钻孔一般与目标矿化构造(1号、2号和3号矿脉,见图3)相交。West Garida钻探的所有矿化截获均载于附录A,重要交叉点见上文表4。钻探在很大程度上证实了浅层倾斜矿化构造的存在和连续性,但没有复制粗含金构造地表采样的高品位,也没有复制WGP-003孔的结果(见日期为2022年9月1日的新闻稿)。
Abu Gaharish
阿布·加哈里什
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 |
领座标系1,2 |
EOH深度(米) |
浸渍 |
栅格方位角 |
评论 |
||
X |
是的 |
Z |
|||||
GHP-001 |
564503.2 |
2917326.1 |
481.7 |
200个 |
-53.1 |
79.6 |
主区 |
GHP-002 |
564431.0 |
2917336.0 |
477.3 |
200个 |
-53.4 |
79.0 |
主区 |
GHP-003 |
564372.9 |
2917345.9 |
478.1 |
一百五十 |
-52.0 |
90.9 |
主区 |
GHP-004 |
564307.4 |
2917342.2 |
478.8 |
一百五十 |
-55.6 |
88.5 |
主区 |
GHP-005 |
564239.3 |
2917351.0 |
478.1 |
120 |
-56.5 |
93.0 |
主区 |
GHP-006 |
564488.8 |
2917177.5 |
480.7 |
200个 |
-53.8 |
91.0 |
主区 |
GHP-007 |
564420.8 |
2917179.8 |
479.6 |
200个 |
-55.0 |
90.3 |
主区 |
GHP-008 |
564347.1 |
2917185.3 |
483.0 |
一百五十 |
-55.3 |
90.4 |
主区 |
GHP-009 |
564701.8 |
2916804.0 |
516.5 |
一百五十 |
-54.1 |
90.3 |
Se切变 |
GHP-010 |
564630.2 |
2916659.1 |
533.2 |
120 |
-54.8 |
88.2 |
Se切变 |
GHP-011 |
564406.4 |
2916699.0 |
495.9 |
100个 |
-53.7 |
89.4 |
西南剪切力 |
GHP-012 |
563841.5 |
2916890.5 |
490.6 |
140 |
-49.7 |
70.9 |
网格区 |
GHP-013 |
563919.9 |
2916955.1 |
508.9 |
140 |
-47.7 |
74.9 |
网格区 |
GHP-014 |
563996.0 |
2916983.4 |
501.8 |
140 |
-50.8 |
71.5 |
网格区 |
GHP-015 |
564566.5 |
2917491.7 |
470.6 |
一百五十 |
-53.7 |
88.7 |
主区 |
GHP-016 |
564523.1 |
2917500.6 |
475.4 |
200个 |
-53.4 |
84.3 |
主区 |
GHP-017 |
564447.2 |
2917507.1 |
474.2 |
160 |
-54.0 |
89.7 |
主区 |
GHP-018 |
564562.3 |
2918038.7 |
464.3 |
120 |
-54.5 |
89.9 |
离子浸出异常 |
GHP-019 |
564491.8 |
2918038.3 |
465.3 |
120 |
-55.0 |
90.9 |
离子浸出异常 |
GHP-020 |
564460.4 |
2918197.8 |
462.5 |
120 |
-53.1 |
90.7 |
离子浸出异常 |
GHP-021 |
564392.0 |
2918198.2 |
461.7 |
120 |
-54.7 |
91.4 |
离子浸出异常 |
GHP-022 |
564996.4 |
2918271.1 |
488.2 |
一百五十 |
-54.9 |
105.3 |
NEX静脉带 |
备注:
|
Table 5: Collar details of RC exploration drill holes at Abu Gaharish
表5:阿布·加哈里什的RC勘探钻孔的接箍细节
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.
在这一第一次通过方案中,在Abu Gaharish探区完成了22个钻孔,从GHP-001到GHP-022(图1),总长度为3,300米(表5和图4)。在覆盖范围很广的区域上钻了几个洞c.矿化走向长1.7公里,大致平行于加哈里什碱性花岗岩岩体与周围的变质沉积和变质火山岩包围岩的接触。在加哈里什主带(GHP-001至GHP-008和GHP-015至GHP-017)上钻了11个孔,以测试围岩包内的剪切构造(GHP-009至GHP-011),钻了3个孔以测试主带西南可能存在的网状和席状脉带,以及在加哈里什岩体本身(GHP-012至GHP-014)内,钻了4个孔以测试离子浸出瓦迪沉积物地球化学异常(GHP-018至GHP-021),最后一口井是为了测试沿着主带走向和东北偏北方向(GHP-022)的东北延伸(NEX)矿脉结构。所有钻孔的卡箍位置如图4所示。
Figure 4: Abu Gaharish drill hole collar plan
图4:阿布·加哈里什钻孔卡箍平面图
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.
来自Abu Gaharish钻探的所有矿化截获物都在附录B中提供,重要的交叉点如表6所示。钻探发现了一个广泛的矿化包层c.与主区有关的350米走向长度,包含较高品位的构造,返回的截距包括2M@8.16g/t Au和3m@4.61g/t Au。对一个1M样品的屏幕火法分析表明,这些区域中存在粗金。围岩中的南向剪切构造返回了较窄的低品位截距,GHP-012孔中较宽的低品位间隔表明,主带西南部可能存在席状脉型减少与侵入体相关的金矿(“RIRG”)型矿化。
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 |
交叉点(M) |
化验(Ppm) |
评论 |
||||||
从… |
至 |
间隔 |
Au |
银 |
CU |
铅 |
锌 |
||
GHP-001 |
1 |
5. |
4. |
2.70 |
2.2 |
69 |
一百九十三 |
181 |
主区 |
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 |
主区 |
GHP-006 |
80 |
83 |
3. |
3.27 |
5.9 |
47 |
一百九十九 |
三九四 |
主区 |
和 |
124 |
126 |
2. |
3.52 |
8.1 |
58 |
126 |
359 |
|
GHP-007 |
8个 |
10 |
2. |
3.78 |
1.3 |
14. |
190 |
188 |
主区 |
GHP-015 |
11. |
13个 |
2. |
2.98 |
4.1 |
40岁 |
200个 |
三百二十九 |
主区 |
和 |
49 |
50 |
1 |
4.77 |
- |
- |
- |
- |
屏幕火试金,粗金存在 |
GHP-016 |
37 |
42 |
5. |
1.23 |
0.5 |
14. |
26 |
一百零二 |
主区 |
和 |
49 |
52 |
3. |
4.61 |
14.8 |
一百八十六 |
967 |
849 |
Table 6: Significant intersections from Abu Gaharish
表6:阿布加哈里什的重要十字路口
Sampling and analytical procedures
取样和分析程序
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孔的直径为53⁄4“或51⁄2”,将块状冲击切屑样本每米直接从旋风分离器收集到预先写入的大塑料袋中,标有孔数和孔深,并在钻探现场顺序铺设。在钻井的每一米之间,旋风分离器和顶盒被压缩空气清理干净。这些袋子是由艾顿地质学家记录在钻探现场的。对散装的100万个样品称重,然后由Aton现场工作人员通过三层分离器进行Riffle裂解,产生大约1/8的裂解,收集在布袋中,编号并标记孔数和深度。在每个样品之间用压缩空气清洁分离器。从最初的散装裂解中产生的废品被重新装袋、贴上标签和标签,并保留在钻探现场。每米的代表性样本被清洗并储存在标有标记的塑料芯片托盘中,每个托盘包含20米的样本,拍照并保留在现场,作为钻孔的永久记录。
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.
然后,将100万个分开的样品,每个重约5千克,运输到罗德鲁鲁样品处理设施,在那里它们被分成两个单独的子样品,重约2.5千克。其中一个样本被标记和贴上标签,并保留在实验室储存。然后,将第二个100万个子样本组合成4M个重约10公斤的复合样本。它们完全混合在一起,再一次混杂在一起,产生名义上的c.250-500克4M复合样品,送至ALS Minerals进行分析。同样,在每个样品之间用压缩空气清洁分离器。这400万个复合样本被分配了新的样本号。处理了4M复合材料试件的散装废品。将QAQC样品以每60个样品约1个认证标准物质(或“标准”样品)、每30个样品1个空白样品、以及每30个样品1个现场复制分离样品的速率插入4M复合样品流中。
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).
这400万个复合样品被运往埃及Marsa Alam的ALS Minerals样品制备实验室,在那里它们被粉碎成超过85%的粒度分数,超过75微米。从这种粉碎的材料中分离出另一个亚样,标称为c.50克大小,运往罗马尼亚罗西亚·蒙大拿的ALS Minerals进行分析。用火焰原子吸收光谱仪(AAS)(分析代码Au-aa23)分析了4M复合样品中的金。任何高品位样品(Au>10g/t)都用分析代码Au-GRA21重新分析(也是火试,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的最终4M复合化验结果后,保留的1M个子样本中的一些由高级Aton地质学家选择重新进行化验,与被认为有意义的4M个复合化验相对应。选择的100万个子样本再次进行抽签分裂,以产生标称c.250-500g 1M拆分样本,再次分配新的样本号。这些样品被送往ALS Minerals,在Marsa Alam进行同样的样品制备,并在Rosia Montana进行后续分析。从100万个子样分离出来的大块废品被重新打包,并保留在现场储存在罗德鲁鲁。QAQC样本以大约每30个样本1个标准、每15个样本1个空白样本、以及每15个样本1个现场复制分裂样本的速率插入到1M分裂样本流中。
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(分析代码Au-aa23)再次分析了这100万个分开的样品中的金,并使用王水消化和原子吸收光谱分析(分析代码AA45)分析了银、铜、铅和锌。任何高品位黄金样品(Au>10g/t)再次使用分析代码Au-GRA21(也是火试金,重量法)进行重新分析。任何高品位的银和贱金属样品(银>100克/吨,铜、铅和锌>10,000ppm或>1%)都用矿石品位技术AA46(也是王水消化和原子吸收光谱分析)重新分析。
All intersections herein reported relate to 1m split samples.
本文报告的所有交叉点都涉及100万个分离样本。
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. |
关于艾顿资源公司 Aton Resources Inc.(AAN:TSX-V)专注于其100%拥有的Abu Marawat特许权(“Abu Marawat”),该特许权位于埃及的阿拉伯-努比亚盾牌,位于Centamin世界级Sukari金矿以北约200公里处。Aton已在Abu Marawat确定了许多金矿和贱金属勘探目标,包括西部的Hamama矿床、东北部的Abu Marawat矿床以及特许权南部的高级Rodruum勘探前景。两座历史悠久的英国金矿也位于巴基斯爵士和塞姆纳的特许权上。Aton已在Abu Marawat确定了几个不同的地质趋势,这些趋势显示出开发各种类型的贵金属和贱金属矿化的潜力。阿布马拉瓦特距离447.7公里2.酒店占地面积大,地处基础设施完善的地区;附近有一条四车道骇维金属加工、一条220千伏输电线和一条输水管道,赫尔加达和卢克索的国际机场也是如此。 |
有资格的人 本新闻稿中包含的技术信息由Aton Resources Inc.勘探经理Javier Orduña BSC(荣誉),MSC,MCSM,DIC,MAIG,SEG(M)编写。Orduña先生是National Instrument 43-101矿产项目披露标准下的合格人员(QP)。 |
本新闻稿中包含的一些陈述是前瞻性陈述。由于前瞻性陈述涉及未来的事件和情况,因此它们本身就涉及固有的风险和不确定因素。每一种情况的实际结果都可能与此类陈述中目前预期的结果大不相同。 |
Appendix A - Significant intersections from the West Garida prospect
附录A-西加里达前景的重要交叉口
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 |
交叉点(M) |
化验(Ppm) |
评论 |
||||||
从… |
至 |
间隔 |
Au |
银 |
CU |
铅 |
锌 |
||
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个 |
八百七十五 |
|
WGP-009 |
72 |
75 |
3. |
0.68 |
2.4 |
151 |
24个 |
2821 |
|
WGP-010 |
28 |
29 |
1 |
1.37 |
1.2 |
84 |
一百五十五 |
八百七十五 |
|
和 |
35岁 |
36 |
1 |
2.03 |
1.6 |
35岁 |
23个 |
一百六十四 |
|
WGP-011 |
24个 |
25个 |
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 |
- |
- |
- |
- |
- |
- |
- |
- |
国家安全局>0.06克/吨Au |
WGP-014 |
- |
- |
- |
- |
- |
- |
- |
- |
国家安全局>0.04克/吨Au |
WGP-015 |
- |
- |
- |
- |
- |
- |
- |
- |
国家安全局>0.17克/吨Au |
WGP-016 |
- |
- |
- |
- |
- |
- |
- |
- |
国家安全局>0.20克/吨Au |
WGP-017 |
23个 |
25个 |
2. |
1.79 |
33.2 |
五百零九 |
497 |
3595 |
|
WGP-018 |
21岁 |
22 |
1 |
3.25 |
24.0 |
221 |
2870 |
3,100 |
|
WGP-019 |
25个 |
26 |
1 |
1.90 |
18.6 |
106 |
1445 |
1360 |
|
WGP-020 |
- |
- |
- |
- |
- |
- |
- |
- |
国家安全局>0.04克/吨Au |
WGP-021 |
32位 |
34 |
2. |
0.32 |
1.1 |
一百五十六 |
35岁 |
2240 |
|
WGP-022 |
21岁 |
22 |
1 |
0.40 |
0.3 |
45 |
8个 |
299 |
|
和 |
33 |
34 |
1 |
0.36 |
0.8 |
54 |
13个 |
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个 |
22 |
2. |
0.70 |
15.7 |
527 |
八四七 |
1870 |
|
WGP-025 |
26 |
27 |
1 |
0.55 |
24.0 |
242 |
819 |
1,705 |
|
备注:
|
Appendix B - Significant intersections from the Abu Gaharish prospect
附录B-阿布加哈里什地区的重要交叉路口
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 |
交叉点(M) |
化验(Ppm) |
评论 |
||||||
从… |
至 |
间隔 |
Au |
银 |
CU |
铅 |
锌 |
||
GHP-001 |
1 |
5. |
4. |
2.70 |
2.2 |
69 |
一百九十三 |
181 |
主区 |
和 |
18 |
19个 |
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 |
主区 |
和 |
98 |
100个 |
2. |
0.79 |
1.2 |
22 |
38 |
48 |
|
和 |
一百一十五 |
116 |
1 |
0.51 |
1.2 |
11. |
35岁 |
58 |
|
GHP-003 |
96 |
九十七 |
1 |
0.50 |
0.9 |
48 |
10 |
65 |
主区 |
GHP-004 |
八十七 |
88 |
1 |
0.63 |
0.7 |
28 |
8个 |
53 |
主区 |
GHP-005 |
12 |
13个 |
1 |
1.03 |
0.8 |
17 |
85 |
32位 |
主区 |
GHP-006 |
68 |
69 |
1 |
0.58 |
0.8 |
14. |
27 |
83 |
主区 |
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个 |
10 |
2. |
3.78 |
1.3 |
14. |
190 |
188 |
主区 |
和 |
54 |
55 |
1 |
0.89 |
2.3 |
八十一 |
148 |
125 |
|
和 |
67 |
68 |
1 |
0.73 |
1.2 |
19个 |
9 |
八十二 |
|
和 |
一百一十二 |
113 |
1 |
0.50 |
0.7 |
15个 |
21岁 |
59 |
|
GHP-008 |
59 |
60 |
1 |
1.13 |
0.5 |
14. |
22 |
58 |
主区 |
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个 |
60 |
一百三十八 |
|
GHP-009 |
- |
- |
- |
- |
- |
- |
- |
- |
国家安全局>0.265克/吨Au(东南切变) |
GHP-010 |
43 |
44 |
1 |
0.64 |
1.2 |
58 |
8个 |
八十二 |
东南向切变 |
GHP-011 |
55 |
57 |
2. |
1.36 |
0.9 |
35岁 |
27 |
111 |
西南切变 |
GHP-0123. |
0 |
29 |
29 |
0.28 |
0.3 |
9 |
15个 |
56 |
网状区,可能是RIRG风格的矿化? |
GHP-013 |
52 |
53 |
1 |
2.50 |
3.4 |
8个 |
29 |
79 |
网格区 |
和 |
75 |
78 |
3. |
0.51 |
0.6 |
8个 |
25个 |
76 |
|
GHP-014 |
- |
- |
- |
- |
- |
- |
- |
- |
美国国家安全局>0.213克/吨Au(网眼区域) |
GHP-015 |
11. |
13个 |
2. |
2.98 |
4.1 |
40岁 |
200个 |
三百二十九 |
主区 |
和 |
17 |
19个 |
2. |
0.89 |
1.9 |
17 |
63 |
136 |
|
和 |
34 |
35岁 |
1 |
1.02 |
1.1 |
21岁 |
77 |
208 |
|
和 |
49 |
50 |
1 |
4.77 |
- |
- |
- |
- |
屏幕火试金,粗金存在 |
和 |
55 |
57 |
2. |
1.60 |
1.3 |
21岁 |
60 |
221 |
|
GHP-016 |
12 |
13个 |
1 |
0.57 |
0.6 |
12 |
106 |
131 |
主区 |
和 |
32位 |
33 |
1 |
0.73 |
0.8 |
13个 |
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 |
交叉点(M) |
化验(Ppm) |
评论 |
||||||
从… |
至 |
从… |
至 |
从… |
至 |
从… |
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 |
主区 |
和 |
119 |
120 |
1 |
1.35 |
0.6 |
3. |
90 |
324 |
|
和 |
123 |
125 |
2. |
0.65 |
0.9 |
15个 |
30个 |
66 |
|
GHP-018 |
- |
- |
- |
- |
- |
- |
- |
- |
美国国家安全局>0.099克/吨Au(IL异常) |
GHP-019 |
- |
- |
- |
- |
- |
- |
- |
- |
美国国家安全局>0.117克/吨Au(IL异常) |
GHP-020 |
- |
- |
- |
- |
- |
- |
- |
- |
美国国家安全局>0.175克/吨Au(IL异常) |
GHP-021 |
- |
- |
- |
- |
- |
- |
- |
- |
美国国家安全局>0.144克/吨Au(IL异常) |
GHP-022 |
- |
- |
- |
- |
- |
- |
- |
- |
NSA>0.109克/吨Au(NEX静脉) |
备注:
|
SOURCE: Aton Resources, Inc.
资料来源:艾顿资源公司