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Gold Science and Technology ›› 2013, Vol. 21 ›› Issue (5): 28-33.

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The Ore-controlling Factors and Prospecting Indicator of Qingshuiquan Gold Deposit in Xinjiang Province

ZHAO Haibin，TIAN Hongbiao，ZHANG Xibing，WEI Dingjun，TIAN Lu   

  1. No.8 Gold Geological Party of CAPF，Urumqi   830057，Xinjiang，China
  • Received:2013-04-03 Revised:2013-06-23 Online:2013-10-28 Published:2014-04-02

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Abstract:

Qingshuiquan gold deposit is located in the west of gold and polymetallic ore belt，Kalamaili metallogenic belt in eastern Junggar，and outputted between Qingshui-Sujiquan big break and Kalamaili deep faults.In this region，the violent tectonic activities and the secondary faults and fracture development which constitute a strongly altered cataclasite zone mainly along northwest direction.Magmatic activity is frequent.Laoyaquan rock is distributed in the north and showed rock foundation appearance，which is powerful heat source for the migration of activated metals enrichment in the region.Outcropping strata are mainly middle Carboniferous Qingshui Formation which is a shallow metamorphic rock，has accepted the latter strongly deformed and metamorphosed，and developmental the boudin and shear fold.Qingshuiquan gold deposit is a broken altered rock-quartz vein type deposits.Ore bodies are banded and lenticular which occur in the secondary structure group intersected at nearly EW main structural system.Ore enrichment is uneven，its morphology，distribution and mineralization enrichment controlled by the stratigraphy and structure closely，and also related to the magmatic activity.It is the main prospecting for the gold-bearing geological，the tectonics and dikes and the alteration.

Key words: ore-controlling factors, prospecting indicator, plastic deformation, Qingshuiquan gold deposit, Xinjiang Province

CLC Number: 

  • P618.51

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