摘要
综述了高压超高压变质岩带的基本构造特征，认为运用体粘滞性流变学理论可以很好地解释高压超高压变质岩的发育过程及其抬升－剥露动力学机制。
This paper describes the basic structural characteristics of the high-pressure and ultrahigh-pressure metamorphic rocks. It is suggested that the exhumation dynamic mechanism and development of the high-pressure and ultrahigh-pressure metamorphic rocks may well be explained by the principle of the bulk viscous rheology.
出处
《地质科技情报》
CAS
CSCD
北大核心
1995年第2期12-16,共5页
Geological Science and Technology Information
基金
国家计委-地矿部重点专项基金
关键词
变质岩
动力学
流变学
岩石学
high-pressure and ultrahigh-pressure metamorphic rock, thick orogenic wedge,bulk viscous rheology, uplift dynamics
