摘要
将四川地貌格局分为三大单元:东部的四川盆地,西部的高山高原和西南部的中山宽谷,并分析了这三大单元的地势差异、地貌结构和发育过程.作者认为,新构造运动形成的构造地貌,决定了四川地貌的宏观格局.
This paper divides landforms in Sichuan province into 3 geomorphical parts: the Sichuan basin in the east part, high mountains and plateau in the west part, and mid-mountains and wide-valley in the southwest part, and analyses their differences of relief, structures of landforms and evolutional process. The author holds that the landforms pattern in Sichuan is established by tectonic landforms that formed in the neotectonic movement.
出处
《西南师范大学学报(自然科学版)》
CAS
CSCD
1991年第3期384-388,共5页
Journal of Southwest China Normal University(Natural Science Edition)
关键词
地貌格局
四川
新构造运动
地貌
landforms pattern
neotectonic movement
Sichuan province