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J4 ›› 2007, Vol. 15 ›› Issue (3): 19-23.

• article • Previous Articles     Next Articles

Geological Features and Prospecting Direction of Duhuangling Gold Deposit, Jilin

 HUAI  Bao-Feng, WANG  Xiao-Yong, SONG  Bing-Jian, LIANG  Hai-Jun   

  1. No. 3 Gold Geological Party of CAPF, Harbin 150049, China
  • Received:2007-04-11 Revised:2007-05-13 Online:2007-06-28 Published:2011-07-28

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Abstract:

Duhuangling gold deposit occurred within the quartz diorite of Late Yanshan Epoch. The ore-bodies are directly controlled by NEE. trending fault structure zone and the eryptoexplosion beccia pipes. According to the morphotype, occurence, size and grade of the orebody, ore types, mineral association and fabric, division of the mineralization periods and stages, wall rock alteration, enriched law of gold, the geological features of eaepiabu gold deposit are illustrated and the genesis of the deposit is preliminary discussed. Th is is a meso-epithermal alteration type gold deposit which related with subvolcanic rock of Late Yanshan Epoch. Based on the prospecting criteria in the area, the exploration direction in the deep and peripheral deposit is pointed out.

Key words: Gold deposit, Geological feature, Prospecting direction, Duhuangling Jilin

CLC Number: 

  • P612

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