| 注册
首页|期刊导航|现代地质|安徽巢湖—滁州地区中生代构造变形特征

安徽巢湖—滁州地区中生代构造变形特征

刘文灿 李博文 潘宝友 刘玉宝

现代地质2001,Vol.15Issue(1):13-20,8.
现代地质2001,Vol.15Issue(1):13-20,8.

安徽巢湖—滁州地区中生代构造变形特征

CHARACTERISTICS OF DEFORMATION DURING MESOZONIC ERA IN THE CHAOHU-CHUZHOU REGION,ANHUI PROVINCE

刘文灿 1李博文 2潘宝友 1刘玉宝1

作者信息

  • 1. 中国地质大学 地球科学与资源学院,
  • 2. 中国地质大学 材料科学与工程学院,
  • 折叠

摘要

Abstract

The Chaohu-Chuzhou region, Anhui Province, located in thesoutheast of Zhangbaling thrust belt, is characterized by highly structural deforming during Mesozonic Era. The main structural pattern is featured by NE-to NNE trending folds and thrusts and was formed during early Indosinian orogene, while NWW-to E-W trending folds were formed during late Indosinian orogene. Yanshanian deformation of the region is characterized by brittle faulting and sedimentary basin formation, which is closely related to the Tanlu Fault activity.

关键词

构造变形/中生代/巢湖—滁州地区/安徽

分类

天文与地球科学

引用本文复制引用

刘文灿,李博文,潘宝友,刘玉宝..安徽巢湖—滁州地区中生代构造变形特征[J].现代地质,2001,15(1):13-20,8.

基金项目

中国黄金学会委托项目( ()

现代地质

OACSCD

1000-8527

访问量0
|
下载量0
段落导航相关论文