地球科学进展 ›› 1994, Vol. 9 ›› Issue (1): 1 -7. doi: 10.11867/j.issn.1001-8166.1994.01.0001

干旱气候变化与可持续发展    下一篇

大地貌学研究进展综述
程绍平,杨桂枝   
  1. 国家地震局地质研究所 北京 100029
  • 收稿日期:1993-02-20 出版日期:1994-01-01
  • 通讯作者: 程绍平

REVIEW ON THE RESEARCH ADVANCES IN MEGA-GEOMORPHOLOGY

Cheng Shaoping,Yang Guizhi   

  1. Institute of Geology,State Seismological Bureau,Beijing 100029
  • Received:1993-02-20 Online:1994-01-01 Published:1994-01-01

板块构造革命和空间影象新技术推动了80年代大地貌学的更新。大地貌学研究的是由板块构造作用和随后的地表侵蚀和沉积作用产生的典型地貌。目前,它在被动大陆边缘、板块边界和活动大陆边缘、以及大陆测高法方面取得了令人瞩目的研究进展。

Plate tectonic revolution and new space image technique had promoted the renewal of mega-geomorphology in the 1980's. Mega-geomorphology studies the typical landforms produced by the plate tectonic processes and the subsequent erosion and sedimentation.Currently,it has a noticeable research advance in passive continental margins, plate boundaries and active continental marins,and continental hypsometry.

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