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.%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(诺利椚鹛嫫*)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.
展开▼
