Application of wide-field electromagnetic method for skarn-type polymetallic deposits' exploration in the Yemaquan, Qinghai Province, China

被引:0
|
作者
Wang, Jinhai [1 ,2 ,3 ,4 ]
Pan, Tong [5 ]
Li, Diquan [1 ,2 ,3 ]
Zhang, Heng [6 ]
Zhan, Jun [4 ]
机构
[1] Cent South Univ, Key Lab Metallogen Predict Nonferrous Met & Geol E, Minist Educ, Changsha 410083, Peoples R China
[2] Cent South Univ, Key Lab Nonferrous & Geol Hazard Detect, Changsha 410083, Peoples R China
[3] Cent South Univ, Sch Geosci & Infophys, Changsha 410083, Peoples R China
[4] Third Geol Explorat Inst Qinghai Prov, Xining 810000, Peoples R China
[5] Bur Geol Explorat & Dev Qinghai Prov, Xining 810000, Peoples R China
[6] Shandong Univ, Inst Geotech & Underground Engn, Jinan 250061, Peoples R China
关键词
wide-field electromagnetic method; CSEM; skarn-type polymetallic deposits; Yemaquan; COPPER-DEPOSIT; INVERSION; CSAMT;
D O I
10.1093/jge/gxaf003
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The Qimantag region in the East Kunlun Mountains is a significant skarn-type polymetallic metallogenic belt in China. With the exhaustion of shallow deposits due to extensive geological and exploration work, there is a pressing need to explore deeper buried ore bodies. The desert soil cover limits the effectiveness of geological and geochemical surveys. Traditional magnetic and gravity surveys have been the primary methods for early exploration but are inadequate for deep exploration. This study applies the Wide-field Electromagnetic Method (WFEM) to mineral exploration in the Yemaquan area of Qimantag region. Developed from the Controlled Source Audio-frequency Magnetotellurics (CSAMT), WFEM uses a vertical or horizontal dipole source to generate electromagnetic responses. It calculates apparent resistivity from a single observed parameter, significantly reducing data acquisition costs. The method is especially effective for identifying deep metal deposits under thick cover. WFEM data were recorded and then processed using the Gauss-Newton method for 2D inversion, followed by 3D kriging interpolation to generate a resistivity model at a depth of 1000 meters in the study area. The results revealed the distribution and contact relationships of sedimentary strata and rock bodies, correlating well with existing geological and geophysical data. Drilling verified the presence of iron, copper, and other polymetallic ore bodies, demonstrating the potential of WFEM for mineral exploration in areas with weak magnetic anomalies. This study validates the effectiveness of WFEM in detecting deep polymetallic deposits in the Qimantag area and provides valuable reference for future exploration in similar geological environments.
引用
收藏
页码:357 / 365
页数:9
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