2011Non-ferrous Mining and MetallurgyRequires access

The geological characteristics of the Qiaohuotexinxin Copper Deposit of Hejing County,Xinjiang province

Sun Jie

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Abstract

The Qiaohuotexinxin Copper Deposit of Hejing County in Xinjiang province is located in the Nalati mineralization belt of western Tianshan.The Upper Bayinbuluke Group of Upper Silurian is the main stratum of this area,Quaternary strata distributes in the low-lying parts of the area.On the north side of the mine area is Nalati piedmont fracture(belong to the branch of Nalati deep fault),the fault structures in the mine area develop well and can be divided into two groups: near E-W,NE-SW,between which the group near E-W is more important.According to geological background and features of Ore Deposit,we conclude occurrence characteristics of ore body,ore type,genesis of the depositand Ore-controlling factors.

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What this paper is about

The Qiaohuotexinxin Copper Deposit of Hejing County in Xinjiang province is located in the Nalati mineralization belt of western Tianshan.The Upper Bayinbuluke Group of Upper Silurian is the main stratum of this area,Quaternary strata distributes in the low-lying parts of the area.On the north side of the mine area is Nalati piedmont fracture(belong to the branch of Nalati deep fault),the fault structures in the mine area develop well and can be divided into two groups: near E-W,NE-SW,between which the group near E-W is more important.According to geological background and features of Ore Deposit,we conclude occurrence characteristics of ore body,ore type,genesis of the depositand Ore-controlling factors.

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Available abstract

The Qiaohuotexinxin Copper Deposit of Hejing County in Xinjiang province is located in the Nalati mineralization belt of western Tianshan.The Upper Bayinbuluke Group of Upper Silurian is the main stratum of this area,Quaternary strata distributes in the low-lying parts of the area.On the north side of the mine area is Nalati piedmont fracture(belong to the branch of Nalati deep fault),the fault structures in the mine area develop well and can be divided into two groups: near E-W,NE-SW,between which the group near E-W is more important.According to geological background and features of Ore Deposit,we conclude occurrence characteristics of ore body,ore type,genesis of the depositand Ore-controlling factors.

Key concepts: Geology, Stratum, Mineralization (soil science), Copper ore, Geochemistry, Mining engineering, Group (periodic table), Fault (geology)

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