大红山铁铜矿区构造体系及矿体空间展布分析  

Tectonic system and ore body spatial distribution of Dahongshan iron-copper mining area

作　　者：姚巍 陈珲 

机构地区：[1]广东省地质局七○六地质大队,广东韶关512028

出　　处：《吉林地质》2012年第2期38-41,共4页Jilin Geology

摘　　要：大红山铁铜矿区位于川滇经向构造体系、南岭纬向构造体系的复合部位,东西向构造是研究区内最基本的构造形式,控制着"大红山式"铁铜矿的分布。本文通过研究各个构造体系的时空演化特征来分析构造体系与矿体的空间展布关系。Dahongshan iron-copper mining area is located in the composite parts of Sichuan-Yunnan longitudinal tectonic system and Nanling latitudinal tectonic system,the most basic tectonic form of the study area is EW trend tectonic,controlled the distribution of ＂Dahongshan type＂ iron-copper ore.This paper studies the temporal evolution characteristics of the various tectonic systems,and analyzes the relationship of tectonic system and ore body spatial distribution.

关 键 词：大红山铁铜矿 基底构造 盖层构造 构造体系 

分 类 号：P618.41[天文地球—矿床学]