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湖北随州荞麦冲金矿地球化学特征
引用本文:杨明银,李书涛.湖北随州荞麦冲金矿地球化学特征[J].资源环境与工程,1998(2).
作者姓名:杨明银  李书涛
作者单位:湖北省地质科学研究所(杨明银),湖北省第八地质大队(李书涛)
基金项目:湖北地勘局科技发展基金!96-0281-16010070
摘    要:对养麦冲金矿进行岩石化学、元素地球化学、包裹体、同位素、稀土元素地球化学研究,揭示了燕山期脆-韧性剪切变形变质作用在金矿成矿过程中的主导作用。矿床成矿期三分,以中期为主,该期成矿环境以温度、氧逸度增高,压力、密度降低为特征,属弱酸-弱碱性介质,弱还原环境。

关 键 词:荞麦冲  金矿  脆-韧性剪切带  地球化学

GEOCHEMICAL CHARACTERISTICS OF QIAOMAICHONG GOLD DEPOSIT IN SUIZHOU, HUBEI
Yang Mingyin, Li Shutao.GEOCHEMICAL CHARACTERISTICS OF QIAOMAICHONG GOLD DEPOSIT IN SUIZHOU, HUBEI[J].Resources Environment & Engineering,1998(2).
Authors:Yang Mingyin  Li Shutao
Affiliation:Yang Mingyin; Li Shutao (Hubei Institute of Geosciences) (No. 8 Geological Team of Hubei Province)
Abstract:By means of studying petrochemistry and geochemitry of inclusion, isotope and element including REE in Qiaomaichong gold deposit, it is revealed that the brittle-ductive shear deformation and metamorphsim play a leading role in the process of the gold metallogenesis and the principal metallogenic epoch is in the medium stage in weak reduction environment with weak acid-weak alkaline medium characterized by higher temperature, higher oxygen fugacity, lower pressure and lower density.
Keywords:Qiamaichang gold deposit brittle ductive shear belt geochemitry  
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