摘要
综述了褶皱—冲断构造的几何特征,造山带的岩石物理性质以及临界锥体力学分析研究现状,认为运用临界锥体力学原理可以很好地解释褶皱—冲断构造发育和发展动力学机制。
This paper discribes the geometrical characteristics of the fold-thrust tectonics and the physical properties of rocks in orogenic belts, and then reviews the mechanical analytical research of the critical wedges. It is suggested that dynamical mechanism of fold-thrust development may well be explained by the principle of the critical wedge mechanics.
出处
《地质科技情报》
CAS
CSCD
北大核心
1993年第3期13-17,共5页
Geological Science and Technology Information
关键词
褶皱
冲断构造
增生作用
造山带
fold-thrust tectonics, critical wedge, accretion, orogenic belt
