首页 | 本学科首页   官方微博 | 高级检索  
     

纵弯叠加褶皱地区岩石有限应变特征:以川东北地区典型叠加褶皱为例
引用本文:黄继钧. 纵弯叠加褶皱地区岩石有限应变特征:以川东北地区典型叠加褶皱为例[J]. 地质论评, 2000, 46(2): 178-185
作者姓名:黄继钧
作者单位:成都理工学院地质学系,610059
基金项目:中国科学院资助项目,4870158,
摘    要:纵弯叠加褶皱地区岩石有限应变特征是所受历次变形的综合结果.远离叠加区应变型式的伸长方向与褶皱轴向一致而缩短方向与褶皱轴垂直,叠加区应变型式不规则,且应变椭球伸长量和缩短量之差值较小.

关 键 词:纵弯褶皱 褶皱叠加 岩石有限应变 应变椭球体

The Features of Finite Strain of Rocks in the Superimposition Fold Area Under Buckling in Northeast Sichuan Province
Huang Jijun. The Features of Finite Strain of Rocks in the Superimposition Fold Area Under Buckling in Northeast Sichuan Province[J]. Geological Review, 2000, 46(2): 178-185
Authors:Huang Jijun
Abstract:The features of rock finite strain in the superimposed fold area under buckling are comprehensive results of multiphase deformation. The stretching direction of the strain far away from the superimposed area is congruent with the axes of the fold, and the shortening direction is vertical to fold axes. The strain pattern in the superimposed area is irregular, and the difference between the stretching and shortening amounts of the strain ellipsoid is reletively small.
Keywords:buckle fold  fold superimposition  finite strain of rocks  strain ellipsoid  
本文献已被 CNKI 维普 万方数据 等数据库收录!
点击此处可从《地质论评》浏览原始摘要信息
点击此处可从《地质论评》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号