昂武隐伏深断裂及其递进变形与区域地质演化特征  

Evolution Feature of Regional Structure of Angwu Concealed Deep Fault and Its Progressive Deformation,Guizhou

作　　者：周启永 

机构地区：[1]贵州省区域地质调查研究院,贵阳550005

出　　处：《贵州地质》1999年第3期199-206,194,共9页Guizhou Geology

摘　　要：从地质、地球物理、地球化学等方面拟定了昂武隐伏深断裂 ,阐明了其主要地质特征和构造演化。初步研究了基底古构造体系的递进变形对区域沉积作用、岩浆作用、上层构造地应力作用和矿化富集作用等区域地质演化的控制作用 ,重点对区域构造的运动学和动力学特征作了初步分析。强调了基底古构造体系研究对区域地质矿产调查的重要意义。Based on the various data in geology.and geoghysics and geochemistry and the author makes a draft of the concealed deep fault of Angwu area,and expounds its geological feature and structural evolution. The controls on the evolution of regional geology such as the progressive deformation of basic palaeotectonic system acting on the regional sedimentation,the magmatism ,the superstructure natural stress and the mineralized concentration are discussed initially.Especially the kinematics of regional structure and its feature are analyzed.This study of basic palaeotectonic system may be a guide to the investigation of regional mineral products.

关 键 词：隐伏深断裂 递进变形 区域地质演化 断层 

分 类 号：P542.3[天文地球—构造地质学] P554.7[天文地球—地质学]