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。
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.
出处
《大地构造与成矿学》
EI
CAS
CSCD
1999年第4期334-344,共11页
Geotectonica et Metallogenia
关键词
剥离断层
构造岩带
控矿作用
成矿模式
湘东北
denudational fault
control on mineraliztion
tectonite zone
model for ore formation
northeastern Hunan
