CAJ | 학술논문

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.
귀주적인지운동주요발생재만삼첩세아지량기(잡니기)여토륭기(낙리륵미모*)지간,시일장이차이륭승위주겸유미약습추적구역성구조운동.해운동미합료선기활동성불동적각개지괴,사타문성위동보연진적통일대륙,시화분지사발전계단적중요사건.
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.