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Chronological Study of Tectonism and Mineralization in Wulonggou Gold Deposit, Eastern Kunlun
Author(s) -
KOU Linlin,
ZHANG Sen
Publication year - 2014
Publication title -
acta geologica sinica ‐ english edition
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 61
eISSN - 1755-6724
pISSN - 1000-9515
DOI - 10.1111/1755-6724.12375_30
Subject(s) - geology , citation , geochemistry , mineralization (soil science) , library science , china , mineral exploration , mineral resource classification , archaeology , history , computer science , soil water , soil science
gold deposit,which is the largest gold depsit in the eastern Kunlun Orogen. They are in sequence of Yanjingou ductile-brittle shear、Yingshigou-hongqigiu ductile-brittle shear and Sandaoliang-kushuiquan ductile-brittle shear from northwest to southeast.Main gold deposit (gold point) is controlled by the ductile-brittle shear. Author achieved fifteen data with wall rocks and the ores of the ductile-brittle shear. The eight ore samples of the metallogenic epoch ,which come from Hongqigou、 Dachaigou、Heishishan et al, is used to measure with the alpha quartz activation (HAESRDQ) method by the Chengdu University of Technology. The two samples of the ductile-brittle shear Deformation Time is used to measure with Ar-Ar method by the Guangzhou Institute,which come from Yanjingou and Dachaigou ductile-brittle shear.The five samples of reaction material source is used to measure with Pb isotope determination by the geological and physical geological academy of Sciences Chinese,which come from Hongqigou、 Sandaoliang、Yingshigou et al.