GEOLOGY AND GENESIS OF THE SHUANGSANZI Ag-Pb-Zn DEPOSIT IN INNER MONGOLIA

ZHAO Jin-cai; YAN Zhi-qiang; CHI Yong-kun; ZHOU Wen-guang; DONG Cun-jie; YANG Shu-hong

doi:10.13686/j.cnki.dzyzy.2010.02.009

2010 Vol. 19, No. 2

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ZHAO Jin-cai, YAN Zhi-qiang, CHI Yong-kun, ZHOU Wen-guang, DONG Cun-jie, YANG Shu-hong. GEOLOGY AND GENESIS OF THE SHUANGSANZI Ag-Pb-Zn DEPOSIT IN INNER MONGOLIA[J]. Geology and Resources, 2010, 19(2): 134-137,150. doi: 10.13686/j.cnki.dzyzy.2010.02.009

Citation:

ZHAO Jin-cai, YAN Zhi-qiang, CHI Yong-kun, ZHOU Wen-guang, DONG Cun-jie, YANG Shu-hong. GEOLOGY AND GENESIS OF THE SHUANGSANZI Ag-Pb-Zn DEPOSIT IN INNER MONGOLIA[J]. Geology and Resources, 2010, 19(2): 134-137,150. doi: 10.13686/j.cnki.dzyzy.2010.02.009

GEOLOGY AND GENESIS OF THE SHUANGSANZI Ag-Pb-Zn DEPOSIT IN INNER MONGOLIA

No. 108 Geologic Party, Liaoning Bureau of Nonferrous Metal Geology, Shenyang 310013, China

Received Date: 11 May 2010

Revised Date: 24 May 2010

Publish Date: 30 June 2010

Abstract

Abstract

The Shuangsanzi area is located in the southwest end of the Ulanhot-Balinyouqi Cu-polymetal metallogenic belt, where five Ag-Pb-Zn blind orebodies have been found. The orebodies are mainly controlled by the early NEEtrending faults and intensively distributed in and around the pyroclastic breccia. The deposits genetically belong to magmatic hydrothermal type. They occur in a zone of NEE direction, with irregular-shaped geophysical anomaly and rich Ag, Cu, Pb, Zn and As soil anomaly. All of those are important prospecting information and indicators in the area.
- Inner Mongolia /
- Shuangsanzi /
- Ag-Pb-Zn deposit /
- magmatic hydrothermal type /
- geophysical and geochemical exploration indicator /