岩屑地球化学测量在黑龙江省三道湾子浅覆盖区的找矿应用效果

doi:10.11872/j.issn.1005-2518.2022.05.173

Abstract

Abstract:

The Sandaowanzi area is a typical shallow overburden area which hosts numerous gold polymetallic ore deposits in Heilongjiang Province，China.More than 10 gold deposits and ore occurrences have been found in the area，such as Sandaowanzi gold deposit，Beidagou gold deposit，Najinkouzi gold deposit，340 highland gold deposit，Sandaowanzi Nanshan gold deposit，etc.，with great prospecting potential.Many soil geochemical surveys have been carried out in the area，but no prospecting breakthrough has been made.Through the comparative tests of various sampling grids，grain sizes and horizons in the study area，the best geochemical sampling method was confirmed，and the 50 m×50 m gridded rock debris geochemical survey method was adopted.Based on the correlation analysis of geochemical characteristics and element symbiotic assemblage characteristics，and combined with regional ore-forming geological conditions，30 comprehensive anomalies were delineated.The main ore-forming elements Au and Ag are strongly enriched in favorable structural areas.Through anomaly verification，12 gold-silver orebodies and 23 gold orebodies have been found，and 3 prospective areas have been delineated，and good prospecting results have been obtained.The study shows that rock debris geochemical survey in Sandaowanzi area can quickly and accurately delineate the range of mine-ralization alteration and improve the prospecting effect，which is an effective prospecting method.It can provide an important reference for ore prospecting in the same type of forest swamp geochemical landscape area.

Key words: shallow overburden area, rock debris geochemistry, abnormal verification, prospecting area, Sandaowanzi area, Heilongjiang Province

CLC Number:

P618.51

Yupeng ZHANG,Dongyan SHI,Mingqi LV,Chenglu LI,Kun ZHANG,Wei TANG. Application Effect of Rock Debris Geochemical Survey in Prospecting in Sandaowanzi Shallow Overburden Area，Heilongjiang Province[J].Gold Science and Technology, 2022, 30(5): 651-663.

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参数	Au	Ag	As	Bi	Cu	Hg	Mn	Mo	Pb	Sb	Te	W	Zn
X	21.3	0.088	12.44	0.555	20.9	0.138	529.6	2.87	30.6	1.37	0.408	2.09	51.9
Max	30 843.0	103.00	868.0	135.00	930.0	30.400	18 400	255.00	2 025.0	184.00	16.10	64.00	507.0
Min	0.1	0.010	0.40	0.010	1.7	0.001	11	0.12	4.0	0.07	0.01	0.04	2.4
S	1 954.20	0.78	21.75	1.92	52.80	0.56	433.65	5.86	36.67	3.05	0.61	5.75	30.91
Cv	91.80	8.90	1.75	3.47	2.53	4.07	0.82	2.04	1.20	2.23	1.48	2.75	0.60
Q	23.66	1.60	5.18	3.70	0.80	0.02	0.65	5.74	2.04	7.58	0.07	3.48	0.68
T	8.9	0.144	41.90	1.320	35.5	0.280	1514.0	7.38	56.2	4.47	1.380	4.25	116.7

因子	lgBi	lgPb	lgTe	lgMo	lgAs	lgSb	lgHg	lgW	lgAu	lgAg	lgCu	lgZn	lgMn	解释方差累计/%
F1	0.846	0.742	0.610	0.587	0.070	0.014	0.139	-0.061	0.144	0.290	0.194	-0.470	-0.501	20.20
F2	0.103	0.004	0.534	0.053	0.833	0.797	0.750	0.098	0.215	0.068	-0.013	-0.208	-0.244	38.30
F3	0.084	0.095	0.142	0.476	0.269	0.355	-0.142	0.808	0.723	0.640	0.106	-0.021	0.025	54.29
F4	-0.081	-0.057	-0.138	0.003	0.005	-0.060	-0.245	0.028	0.119	-0.017	0.856	0.758	0.661	68.53

编号	面积/km²	ΣNAP	主成矿元素	种数	异常数	成矿条件	序次	评价
Ht-01	5.641	39.58	Au、Ag、As、Hg、W	13	368	极有利	1	矿体引起的异常
Ht-16	5.918	20.77	Au、Ag、As、Sb、Bi	12	297	极有利	2	热液（蚀变）引起的异常
Ht-10	5.002	19.71	Hg、Te、Bi、As、Sb	11	202	极有利	3	热液（蚀变）引起的异常
Ht-17	3.804	13.69	Au、Mo、Cu、Pb	10	116	较有利	4	矿体引起的异常
Ht-13	0.410	2.19	Au、Bi、Ag、Sb	9	30	极有利	5	矿体引起的异常
Ht-15	0.751	2.07	Ag、Pb、Zn、Bi、Cu	9	50	有利	6	异常成因不明
Ht-27	0.139	3.27	Au、Ag、Sb、Pb、Bi	9	18	极有利	7	矿体引起的异常
Ht-06	0.721	1.12	Sb、Hg、Au、As、Pb	10	37	有利	8	异常成因不明
Ht-26	0.163	2.29	Ag、Pb、Hg、Sb、As	7	13	极有利	9	蚀变矿化引起异常
Ht-30	0.251	2.07	Au、Ag、Sb、Cu、W	7	20	极有利	10	矿体引起的异常

异常编号	见矿情况	矿体特征	矿石/围岩	矿物	成矿类型
Ht-26	矿体13条	Ⅰ1斜厚0.4 m，Au品位282.43×10^-6	石英脉/安山玢岩	黄铁矿、碲金矿、黄铜矿	碱性岩型低温热液型
Ht-24	矿体7条	Ⅱ3斜厚8 m，Ag品位74.2×10^-6、Cu品位0.74%	蚀变岩/安山岩	黄铁矿、黝铜矿、重晶石	高硫化低温热液型
Ht-27	矿体3条	Ⅱ8、9斜厚1 m，Au品位1.41×10^-6、1.01×10^-6	蚀变岩/安山岩	黄铁矿、黄铜矿、碳酸盐	高硫化低温热液型
Ht-16	金矿体1条	Ⅸ斜厚28 m，Au品位1.2×10^-6	蚀变岩/安山岩	浸染状黄铁矿	低温热液型
Ht-22	银矿体1条	宽2 m，Ag品位130.77×10^-6	蚀变岩/安山岩	辉锑矿、黄铁矿	低温热液型
Ht-01	矿体10条	Ⅲ1斜厚3.65 m，Au品位6.04×10^-6	石英脉/安山玢岩	黄铁矿、碲金矿、方铅矿	构造—热液叠加型
Ht-01	金矿体2条	均斜厚2 m，Au品位11.22×10^-6、Ag品位5.07×10^-6	石英细脉/安山岩	黄铁矿、自然金	中低温热液型
Ht-01	金矿体4条	Ⅳ1斜厚3 m，Au品位1.19×10^-6、Ag品位64.06×10^-6	石英脉/安山岩	黄铁矿、碲银矿、方铅矿	构造—热液叠加型
Ht-13	金矿体1条	Ⅵ斜厚6 m，Au品位6.05×10^-6	石英脉/变质岩	黄铁矿、磁铁矿、黄铜矿	构造蚀变岩型
Ht-10	金矿体1条	斜厚1 m，Au品位1.05×10^-6、1.14×10^-6	蚀变岩/安山岩	浸染状黄铁矿	低温热液型
Ht-19	金矿点	Au品位2.9×10^-6	石英脉/安山岩	黄铁矿	低温热液型

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Application Effect of Rock Debris Geochemical Survey in Prospecting in Sandaowanzi Shallow Overburden Area，Heilongjiang Province

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