GEOLOGICAL CHARACTERISTICS AND METALLOGENIC MODEL OF SUPER-LARGE KOUNRAD PORPHYRY COPPER DEPOSIT, KAZAKHSTAN

HAN Shuqin; CHEN Xuanhua; YANG Nong; CHEN Zhengle; SHI Wei; Ye Baoying

2010 Vol. 16, No. 2

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HAN Shuqin, CHEN Xuanhua, YANG Nong, CHEN Zhengle, SHI Wei, Ye Baoying. GEOLOGICAL CHARACTERISTICS AND METALLOGENIC MODEL OF SUPER-LARGE KOUNRAD PORPHYRY COPPER DEPOSIT, KAZAKHSTAN[J]. Journal of Geomechanics, 2010, 16(2): 203-212.

Citation:

GEOLOGICAL CHARACTERISTICS AND METALLOGENIC MODEL OF SUPER-LARGE KOUNRAD PORPHYRY COPPER DEPOSIT, KAZAKHSTAN

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijijng 100081, China
2.
China University of Geosciences, Beijing 100083, China

Received Date: 20 May 2010

Publish Date: 25 June 2010

Abstract

Abstract

The Kounrad porphyry copper deposit was discovered 70 years ago in the Balkhash Metallogenic Belt of the Central Asian Metallogenic Domain, . It is a typical super-large porphyry copper deposit developed under the tectonic environment of continental margin arc, with a metallogenic model of granodiorite. The vertical and lateral zonings of the wall rock alteration and ore mineral assemblages are obviously observed in the deposit. High content ore in the leaching zone and the ore deposition at a very shallow depth made it easy to be mined. It is suggested that the metallogenesis of the deposit was controlled by the circular structure, and had a very close relation with the secondary quartzite and argillic alteration.
- Kounrad /
- porphyry copper deposit /
- geological characteristics /
- metallogenic model /
- developing future

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References

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