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Gold Science and Technology ›› 2020, Vol. 28 ›› Issue (6): 837-845.doi: 10.11872/j.issn.1005-2518.2020.06.084

• Mineral Exploration and Resource Evaluation • Previous Articles     Next Articles

Geochemical Characteristics of Stream Sendiments and Exploration Prospective of the Qiujidonggou Gold Deposit in Dulan County,Qinghai Province

Ming LIU1(),Zizhang WANG2()   

  1. 1.Shandong Lunan Institute of Geo-Engineering Exploration (No. 2 Geological Team,Shandong Geological Prospecting Bureau of Geology & Mineral Resources),Jining 272000,Shandong,China
    2.Henan Fifth Research & Design Corporation of CNNC,Zhengzhou 450000,Henan,China
  • Received:2020-05-02 Revised:2020-07-28 Online:2020-12-31 Published:2021-01-29
  • Contact: Zizhang WANG E-mail:1290278570@qq.com;zizhangwang@163.com

Abstract:

The Qiujidonggou gold deposit in Dulan County is located in the middle of the east Kunlun metallogenic province,so it is necessary to carry out research on the reverse side of mineral exploration.The area has developed structures,frequent research activities,and a good metallogenic geological background.There are famous Wulonggou gold deposit and Tanjianshan gold deposit around the mine.Due to the good metallogenic background in this area,the area has attracted the attention of scholars at home and abroad.Most of the previous studies have focused on the geological characteristics of the deposits and the metallogenic age,and there are few studies on regional mineral exploration,which has led to no breakthrough in regional prospecting. Because the mining area is large and the coverage is serious,general physical and chemical exploration methods are difficult to meet the exploration needs,which limits the prospecting and mining work of the mine.In order to reveal the metallogenic characteristics of the ore bodies in the study area and the prospecting direction,this paper explores the 1∶25 000 water system sediments in the Qiujidonggou gold deposit,to explore the mineralization characteristics and delineation of the deposit mine target area.Through research,it is found that the four elements Ag,Pb,As and Sb are highly correlated with metallogenic elements and can be used as indicator elements for metallogenic.Using the method of contrast anomaly delineation,four comprehensive anomalies were delineated in the study area.One type I anomaly is the AS-4 comprehensive anomaly and the second type anomaly is the AS-1 and AS-3 anomalies,third type anomaly is the AS-2 anomalies.This will provide a theoretical basis for the theoretical research and prospecting direction of regional prospecting.

Key words: stream sediment survey, geochemical characteristics, contrast anomaly delineation method, east Kunlun metallogenic province, Qiujidonggou gold deposit, Qinghai Province

CLC Number: 

  • P632

Fig.1

Regional geological map of Qiujidonggou gold deposit in Dulan County"

Fig.2

Element anomaly area and sampling location map of stream sediments in Qiujidonggou gold deposit"

Table 1

Calculation results of lower limit of elemental anomalies of stream sediments in the study area"

元素对数 平均值对数 标准差对数异常下限异常下限反算全区元素均值最终异常下限
Au0.030.220.472.351.412.30
Ag-1.200.14-0.920.110.070.15
Cu1.380.201.7855.5226.7855.00
Pb1.230.111.4525.9717.3828.00
Zn1.810.142.09110.0067.20105.00
As1.060.181.4222.5112.4322.00
Sb0.030.140.311.881.131.80
Hg-1.710.26-1.190.060.020.05
W0.170.190.553.011.623.00
Sn0.460.110.684.442.994.40
Mo0.030.180.392.281.182.30
Ni1.470.171.8158.2331.8658.00
Bi-0.610.15-0.310.430.260.43
V1.930.142.21151.3688.91150.00
Co1.080.161.4023.5012.9524.00
Ti3.520.173.866 384.113 569.396 300.00
Cd-0.720.160.400.360.200.35
Ba2.690.142.97881.79512.35880.00
Te-1.210.14-0.930.100.060.09
Y1.390.111.6137.2425.1738.00

Table 2

Statistical of basic geochemical parameters of geochemical anomaly of stream sediments"

异常编号异常元素异常点数

异常下限

T

峰值

Cmax

异常均值

Caˉ

标准离差

δ

面积(S) /km2

衬度

K==CaˉT

异常规模

D=K·S

AS-1Mo262.305.12.720.550.450.750.34
Cd170.351.200.480.080.380.800.30
Te140.090.140.110.020.200.810.16
Cu1155.00118.0063.8814.370.0380.800.03
Au112.303.002.760.570.0630.770.05
AS-2Mo202.305.402.650.550.921.151.06
Sb161.802.701.810.380.561.010.57
As2222.00126.0044.155.041.942.013.90
Au152.306.402.750.571.191.201.43
Ag80.150.230.180.020.731.200.88
Bi90.431.300.680.090.681.581.07
W143.0022.24.670.690.571.560.89
Cd140.350.620.430.081.231.231.51
Pb1328.0052.334.594.291.221.241.51
Zn4105.00112.00105.521.400.021.010.02
Sn34.405.505.070.730.421.150.48
AS-3Au102.3039.15.430.550.612.361.44
As922.00497.0072.015.040.643.272.09
Hg110.050.700.150.020.583.001.74
Sb11.802.302.300.380.0141.280.02
Cu1655.0092.462.6814.370.341.140.39
Co1624.0038.0029.35.280.601.220.73
Ni1658.0097.1068.2513.180.5631.180.66
Ti246 300.008 894.007 108.251 407.360.541.130.61
V18150.0220.00162.2731.230.331.080.36
AS-4Au82.305.603.450.550.491.800.88
Ag320.1513.100.850.021.155.676.52
Pb3428.00769.0069.164.291.312.473.24
Zn18105.00309.00122.1621.401.041.161.21
W533.0071.306.540.692.062.184.49
Mo152.309.303.210.550.451.400.63
Cu355.00154.00100.7314.370.161.830.30
Sb121.8010.22.930.380.671.631.09
Cd360.352.600.740.081.712.113.61
Ni358.00136.0088.7313.180.111.530.17
As622.00110.0048.385.040.652.201.43
Sn24.45.35.20.730.041.180.05

Fig.3

Analytical chart of anomalies in water system sediments of study area"

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