摘要
贵州的区域构造研究,大致经历了三个阶段,即:槽台观点阶段,地质力学观点阶段,板块观点阶段。本文对前两个阶段仅进行简要的回顾。而对后一个阶段则作为新进展加以介绍。近十年来,人们运用板块观点对贵州的区域构造特征及其演化过程进行了全面深入的探索,较前大大的前进了一步。与此同时,在贵州掀起了推覆构造研究的热潮,这对贵州的区域构造研究也起了一定的推动作用。
The history of regional tectonic study of Guizhou can be divided into three stages, that is, the stage of geosyncline-platform theory, the stage of geomechanics theory and the stage of plate tectonics theory. First two stages are only shortly reviewed in this paper and third stage is introduced in particular as an advance of the regional tectonic study. In recent ten years, the plate tectonics theory has been applied to the deep and synthetical studies of the regional tectonic features and evolution of Guizhou, and has advanced the regional tectonic study to a new stage. Meanwhile, many geologists put their stress on the study of nappe structures in Guizhou, which also has a positive role in advancing the regional tectonic studies of Guizhou.
出处
《贵州地质》
1992年第4期326-330,共5页
Guizhou Geology
