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Gold Science and Technology ›› 2014, Vol. 22 ›› Issue (2): 7-12.doi: 10.3969/j.issn.1005-2518.2014.02.007

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The Controlling of Secondary Detachment Fault for Gold Mineralization in  Western Henan Province:Taking Huaishuping Gold Mine as an Example

MEI Xiujie,ZHANG Canhui,YANG Xiandao,GUO Yuxi   

  1. No.2 Institute of Geological and Mineral Resources Survey of Henan,Zhengzhou   450001,Henan,China
  • Received:2013-11-27 Revised:2014-01-25 Online:2014-04-28 Published:2014-08-26

Abstract:

Huaishuping gold area is located between the Xiong’er Mountain fault and the rift basin of Tantou-Songxian in Cenozoic,research shows that the secondary gentle-dipping faults of gentle dip slip-detachment fault in Meso-Cenozoic has provides the ore-hosting sites for ore-forming of the Huaishuping gold deposit.The Yanshan granite porphyry (or buried porphyry) which revealed has provided the ore-forming fluids.Hydrothermal along veins or fracture rise to secondary gentle-dipping faults and enrichment and mineralization of gold under optimal physical and chemical conditions.The scale of Huaishuping gold deposit has reached large size.The gentle dip slip-detachment fault in Meso-Cenozoic is regional faults and their secondary gentle-dipping faults are widely developed in the south of Songxian and Luoning and so on and offer space for enrichment of metallogenic materials.Comprehensive studies have shown that the secondary gentle-dipping faults on the regional prospecting are very wide.

Key words: granitic porphyry, gentle-dipping faults, slip-detachment fault, geological characteristics, Huaishuping gold deposit, Henan Province

CLC Number: 

  • P618.51

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