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辽西地区中生代构造格局及其形成演化
引用本文:王根厚,张长厚,王果胜,吴正文.辽西地区中生代构造格局及其形成演化[J].现代地质,2001,15(1):1-7.
作者姓名:王根厚  张长厚  王果胜  吴正文
作者单位:中国地质大学 地球科学与资源学院,
基金项目:国家自然科学基金项目(19802019、49702034)。
摘    要:在横穿辽西地区构造变形剖面及重点区段的详细构造解析的基础上 ,结合构造变形、沉积组合、岩浆岩特征及同位素年代学等资料 ,对辽西地区中生代以来的总体构造格局进行了厘定 ,认为辽西地区中生代主要构造格局由印支期的东西向褶皱 -逆冲构造、早燕山期的北东向叠瓦状逆冲推覆构造、晚燕山期早期的北东向“盆 -岭”构造、晚燕山晚期的北北东向左行走滑构造组成

关 键 词:构造格局  逆冲叠瓦构造  盆-岭构造  中生代  辽西地区
文章编号:1000—8527(2001)01—0001—07
修稿时间:2000年10月17

TECTONIC FRAMEWORK OF WESTERN LIAONING PROVINCE AND ITS EVOLUTION DURING MESOZOIC
WANG Gen hou,ZHANG Chang hou,WANG Guo sheng,WU Zheng wen.TECTONIC FRAMEWORK OF WESTERN LIAONING PROVINCE AND ITS EVOLUTION DURING MESOZOIC[J].Geoscience——Journal of Graduate School,China University of Geosciences,2001,15(1):1-7.
Authors:WANG Gen hou  ZHANG Chang hou  WANG Guo sheng  WU Zheng wen
Abstract:Based on the study of two major cross-sections in the westernLiaoning Province,the tectonic framework of the western Liaoning Province consists of four kinds of fault systems with different orientation and deformation time:(1)east-west-trending reverse faults and folds of the Indosinian epoch,(2)northeast oriented imbricate thrust system of the Early Yanshanian,(3)northeast-north striking “basin and range”-type system of the early stage of the Late Yanshanian epoch,(4)north-to northeast trending sinistral strike-slip fault system of the Late Yanshanian epoch.
Keywords:tectonic framework  imbricate thrust fault  basin  range structure  Mesozoic  western Liaoning Province
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