随枣北部地区构造类型及控矿特征  

STRUCTURE IN NORTHERN SUIZHOU - ZAOYANG AND ITS ORE - CONTROL IMPLICATIONS

作　　者：胡起生[1] 

机构地区：[1]湖北省第八地质大队

出　　处：《湖北地矿》2001年第4期38-44,共7页Hubei Geology & Mineral Resources

摘　　要：随枣北部地区构造类型有近水平顺层韧性剪切变形、强烈挤压变形、拆离滑脱构造、逆冲推覆构造和脆性断裂等。拆离滑脱构造和逆冲推覆构造为区内主要控矿构造。据构造控矿特征,文中提出了随枣北部地区构造控矿的成矿系列,对找矿方向作了简单分析。In the northern Suizhou - Zaoyang region exist ductile deformation of subhorizontal bedding shear, intensively compressive deformation, decollement structure, thrust nappe structure, and brittle faults, among which the decollement structure and thrust nappe structure are the major ones. Based on their ore- controlling features, an ore- formation series is proposed for the Suizhou- Zaoyang region. And the further ore- prospeciting targets and region have also been discussed briefly.

关 键 词：构造类型 控矿特征 找矿方向 拆离滑脱构造 逆冲推覆构造 

分 类 号：P612[天文地球—矿床学]