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湘南姑婆山岩体北西侧侵入接触带构造控矿研究
引用本文:余君鹏,秦松贤.湘南姑婆山岩体北西侧侵入接触带构造控矿研究[J].地质科技情报,2007,26(2):25-29.
作者姓名:余君鹏  秦松贤
作者单位:1. 中国地质大学研究生院,武汉,430074
2. 中国地质大学地球科学学院,武汉,430074
基金项目:中国地质调查局区域地质调查项目
摘    要:位于湖南南部的姑婆山岩体北西侧侵入接触带受断裂构造控制明显,表现复杂多样,是该区钨、锡多金属矿床的主要控矿构造.根据接触带不同成矿区段的空间展布特点、构造变形和矿化蚀变特征,认为该区接触带构造是岩体侵位和区域应力双重作用的结果,并首次将该侵入接触带构造划分为3种类型,即侵入接触-断裂复合型、双侵入接触-断裂复合型以及捕虏体接触-断裂复合型.明确提出了侵入接触带构造控矿的观点,从而为进一步研究其成矿及控矿作用提供必要的理论依据.

关 键 词:姑婆山岩体  侵入接触带构造  构造变形  矿化蚀变  湘南
文章编号:1000-7849(2007)02-0025-05
修稿时间:2006-11-15

Intrusive Contact Structures in the Northwest of the Guposhan Pluton, Southern Hunan Province
YU Jun-peng,QIN Song-xian.Intrusive Contact Structures in the Northwest of the Guposhan Pluton, Southern Hunan Province[J].Geological Science and Technology Information,2007,26(2):25-29.
Authors:YU Jun-peng  QIN Song-xian
Institution:1. Graduate School ;2. Faculty of Earth Sciences, China University of Geosciences ,Wuhan 430074, China
Abstract:The main ore-controlling structure of tin,tungsten and other multi-metallic deposit is the complex and diversified intrusive contact structure located in the northwest of Guposhan pluton,southern Hunan Province.The analysis of the characteristics of its spatial distribution,deformation and alteration shows that this structure is formed as the result of emplacement of pluton intrusion and regional tectonic stress.This contact structure is subdivided, for the first time,into three compound types: intrusion with faulting,bi-intrusion with faulting and xenogenic inclusion with faulting.The idea that the intrusive contact structure controls the-body will provide theoretical evidence for the further research of mineralization and ore control.
Keywords:Guposhan pluton  intrusive contact zone structure  structure deformation  alteration  southern of Hunan
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