吉林汪清杜荒岭金矿地质特征及找矿标志探讨

J4 ›› 2007, Vol. 15 ›› Issue (3): 11-14.

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Geological Features and Prospecting Direction of Duhuangling Gold Deposit, Jilin

ZHOU Dian-Yu, SONG Bing-Jian, HUAI Bao-Feng

No.3 Gold Geological Party of CAPF，Harbin 150049，China

Received:2007-04-15 Revised:2007-04-28 Online:2007-06-28 Published:2011-07-28

Abstract

Abstract:

Duhuangling gold deposit occurred in the quartz diorite of Late Yanshan Epoch. The ore-bodies are directly controlled by EW -trending fault structure zone. The main types of the wall-rock alteration include quartzitification, sericitization, chloritization, pyritization, limonitization, kaolinitization, carbonatization. Evolution of the alteration may been divided into three atages, namely, early-mineralizing alteration, middle-mineralizing alteration and late-mineralizing alteration. The gold mineralization is closely mated to the alteration, especially to the quartaitification, pyritization and sericitization-quartzitification. This is a typical fractured alteration type gold deposits. This 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.

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

CLC Number:

P618.102

ZHOU Dian-Yu, SONG Bing-Jian, HUAI Bao-Feng. Geological Features and Prospecting Direction of Duhuangling Gold Deposit, Jilin[J].J4, 2007, 15(3): 11-14.

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