摘要
贵州的印支运动主要发生在晚三叠世亚智梁期(卡尼期)与土隆期(诺利—瑞替期)之间,是一场以差异隆升为主兼有微弱褶皱的区域性构造运动。该运动弥合了先期活动性不同的各个地块,使它们成为同步演进的统一大陆,是划分地史发展阶段的重要事件。
The Indosinian movement in Guizhou occurred as a kind of differential uplifting-dominated regional tectonic movements during the periods between the Carnian and Norian - Rhaetian （ Late Triassic）. This movement contributed to the amalgamation of the pre-existing individual blocks and development of a unified continent, and thus marked an important tectonic event in geologic history.
出处
《沉积与特提斯地质》
CAS
CSCD
2009年第2期100-103,共4页
Sedimentary Geology and Tethyan Geology
关键词
贵州
印支运动
重大事件
Guizhou
Indosinian movement
important event
