泰和盆地构造和演化初探  

A Preliminary Discussion on the Structure and Evolution of the Taihe Basin

作　　者：王迪文 龙天 张永忠 

机构地区：[1]江西地质矿产勘查开发局地矿调研大队

出　　处：《江西地质科技》1997年第4期165-169,共5页

摘　　要：我国大部分地区的小新生代盆地的成生、演化受断裂构造的控制,泰和盆地即是严格受断裂构造控制的走滑拉张型盆地。本文着重从盆地的基底构造、盆缘断裂构造及盆地同生、后期构造阐述了它们与盆地形成和演化的关系。The genesis and evolution of most of the Mesozoic - Cenozoic basins in China arecontrolled by fracture structure, and the Taibe Basin a strike slip extensional basm controlled strictly by fracture structure I his paper highlights the relation of the genesis and evolution of the basm with basement structure , marginal fractures and contemporaneous and deuterogenic structures

关 键 词：盆缘断裂 走滑拉张 形成演化 泰和盆地 盆地 

分 类 号：P542.3[天文地球—构造地质学]