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湘东北思村—砰山剥离断层特征及控矿研究
引用本文:周怡湘,程巨能.湘东北思村—砰山剥离断层特征及控矿研究[J].大地构造与成矿学,1999,23(4):334-344.
作者姓名:周怡湘  程巨能
作者单位:株洲市地矿资源管理局,湖南株洲412008
摘    要:思村一砰山断层是湘东北连云山变质核杂岩构造系统中一条剥离断层。本文结合断层带已知矿床实例,对该断层构造岩带特征、形成与演化机制和控矿作用进行了分析,并对其成矿模式进行了探讨。

关 键 词:剥离断层  构造岩带  控矿作用  成矿模式  湘东北
文章编号:1001-1552(1999)04-0334-11

THE SICUN-PENGSHAN DENUDATIONAL FAULT AND ITS CONTROL ON ORE MINERALIZATION, NORTHEASTERN HUNAN,CHINA
ZHOU Yi-xiang,CHEN Ju-neng.THE SICUN-PENGSHAN DENUDATIONAL FAULT AND ITS CONTROL ON ORE MINERALIZATION, NORTHEASTERN HUNAN,CHINA[J].Geotectonica et Metallogenia,1999,23(4):334-344.
Authors:ZHOU Yi-xiang  CHEN Ju-neng
Abstract:The Sicun-Pengshan fault is one of the denudational faults developed in the tectonic system Of the LianyUn Mt. metamorphic core complex in northeastern Hunan Province, China. The present study on this fault includes the following: the geological characteristics Of tectonite zones developed across the fault, the formational and evolutional mechanism of the fault, and the ore mineralization controlled by the fault. The ore dePOsits associated with the fault have been studied,and a model for ore formation related to the development of the fault is established here.
Keywords:denudational fault  control on mineraliztion  tectonite zone  model for ore formation  northeastern Hunan
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