THE FEATURE OF QINGGANGPING GOLD DEPOSIT AND STUDY ON THE STABIE ISOTOPE, XIONGERSHAN AREA,WESTERN HENAN PROVINCE

Chen Wang; Cui Bo; Xu Mengluo; Guo Shiran

1996 Vol. 5, No. 3

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Article navigation > Geology and Resources > 1996 > 5(3): 213-217

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Chen Wang, Cui Bo, Xu Mengluo, Guo Shiran. THE FEATURE OF QINGGANGPING GOLD DEPOSIT AND STUDY ON THE STABIE ISOTOPE, XIONGERSHAN AREA,WESTERN HENAN PROVINCE[J]. Geology and Resources, 1996, 5(3): 213-217.

Citation:

Chen Wang, Cui Bo, Xu Mengluo, Guo Shiran. THE FEATURE OF QINGGANGPING GOLD DEPOSIT AND STUDY ON THE STABIE ISOTOPE, XIONGERSHAN AREA,WESTERN HENAN PROVINCE[J]. Geology and Resources, 1996, 5(3): 213-217.

THE FEATURE OF QINGGANGPING GOLD DEPOSIT AND STUDY ON THE STABIE ISOTOPE, XIONGERSHAN AREA,WESTERN HENAN PROVINCE

Henan Institute of Nonferrous Metal Mineral Resources and Geology

Received Date: 10 February 1996

Publish Date: 30 September 1996

Abstract

Abstract

Qinggangping deposit is a low-angle altered fractural rock type gold deposit. It is low-angle, thin,high grade and long extending. The study on stable isotopes suggests the metallo-genic material derived from Huashan granite. As other gold deposits in Xiongershan area the deposit is formed by Yanshannian granite. There are metallogenic conditions for middle-large scale gold deposits.
- western Henan /
- Qinggangping /
- gold deposit /
- low-angle type /
- stable isotopes /
- granit