滇黔相邻区银厂坡—石门冲断褶皱带构造特征及构造控矿作用浅析  

The Structural Features and the Structural Control of the Mineralization of Yinchangpo-Shimenchong Zone of Bruchfalten in the Adjacent Area of Guizhou and Yunnan

作　　者：王佳武[1] 杨胜堂[1] 刘爱民[1] 

机构地区：[1]贵州省地矿局一O三地质大队

出　　处：《贵州地质》2008年第1期21-25,共5页Guizhou Geology

基　　金：国土资源大调查项目资助;矿调[2004]5-2

摘　　要：本文在叙述"银厂坡-石门冲断褶皱带"断裂展布样式、构造组合特征基础上,总结了区内构造控矿特征,指出不同级次断裂控制了矿带、矿床及矿体的分布。在此基础上,把"银厂坡-石门冲断褶皱带"分为6个断裂带(矿带),10个构造复杂区(找矿靶区),初步认为"构造化学找矿方法"是区内行之有效的找矿方法。On the base of narrate the unrolling pattern of rupture and the tectonic association feature, it summarizes the structural features of this area, also points out that the rupture of different level control the spread of ore belt, mineral deposit and ore body in this paper. Then it divide Yinchangpo - Shimenchong zone of bruchfaltm into six ruptured zone （ ore belt） , ten structural complex area （target area）, think that the

关 键 词：构造特征 构造控矿 银厂坡-石门冲断褶皱带 滇黔相邻区 

分 类 号：P618.42[天文地球—矿床学] P618.43[天文地球—地质学]