长坡区锡多金属矿床地质特征与成矿条件分析  

Geological characteristics of tin polymetallic deposit in Changpo district and tts ore forming condition

作　　者：范森葵[1] 

机构地区：[1]中南大学地学与环境工程学院

出　　处：《矿产与地质》2006年第4期418-422,共5页Mineral Resources and Geology

摘　　要：长坡区锡多金属矿床位于大厂锡多金属矿田的西矿带,它是在地层、断裂构造和岩浆岩“三位一体”作用下形成的,地层是基础条件,断裂构造起了主导作用,岩浆提供热源以及可能提供了液源甚至矿质。因此,今后找矿中,更应关注断裂构造的研究。Tin polymetallic deposit in Changpo district are located in west ore zone of Dachang tin polymetallic ore field, which is formed under the integrated function of strata, fractures and magmatic rocks, namely stratum is the basic condition while structure played ore conducting function and the magma provided heat source and possible ore liquid or matter. Therefore, the structure research should be paid more attention to in future ore prospecting.

关 键 词：锡多金属矿床 成矿条件 地质特征 长坡 

分 类 号：P618.44[天文地球—矿床学]