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J4 ›› 2007, Vol. 15 ›› Issue (2): 1-8.

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The Geological Features and Controlled - Deposit factors on Daxin Gold Deposit in Hunan

 LIANG  Dong, DAI  Jian-Bin   

  1. No. 11 Part of Gold Army of Chinese Armed Police Force, Ningxiang, Hunan 410600, China
  • Received:2007-03-28 Revised:2007-04-05 Online:2007-04-27 Published:2011-12-07

Abstract:

Daxin gold deposit in Hunan province are hosted by the Sinian gravel - bearing sand-stone slate, and are closely controlled by the faults. The mineralizing stage of these deposits can be divided into two periods: i.e. period of hydrothermal mineralizing and period of epigenic mineralizing, and the former one is the primary mineralizing period. These gold deposits should belong to the type of magmatic hydrothermal gold deposits that were mainly occurred in the fractured altered rocks. Strata, structure/tectonic and magmatism are the three important factors that controlled the formation of Daxin gold deposits.

Key words: gold deposit, controlled - deposit factor, geological features, Daxin, Hunan province

CLC Number: 

  • P618.51

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