地震地质 ›› 1986, Vol. 8 ›› Issue (1): 25-32.

• 科研简报 • 上一篇    下一篇

青藏高原线性构造及其活动特征

郑炳华   

  1. 国家地震局地质研究所
  • 收稿日期:1984-10-31 出版日期:1986-03-05 发布日期:2009-11-25

QINGHAI-XIZANG PLATEAU LINEAMENTS AND THEIR CHARACTERISTIC ACTIVITIES

Zheng Binghua   

  1. Institute of Geology, State Seismological Bureau
  • Received:1984-10-31 Online:1986-03-05 Published:2009-11-25

摘要: 自印度洋板块和欧亚板块汇聚后,特别是上新世以来,青藏高原的地壳又如何活动,一直是人们感兴趣的研究课题。本文试图利用陆地卫星影象具有视域广和连续性的优点,对所提供丰富、清晰的线性信息,着重分析线性构造空间展布及其组合的几何式样,进而结合地质、地震和地球物理资料探讨高原地区地块和块缘断裂活动基本特征及其形成机制。

Abstract: The convergence of Indian and Eurasian plates,especially the crustal activity in the Qinghai-Xizang Plateau has attracted geoscientists attention.This paper atempts to use the advantage of wide-sight and continuity of view on the Landsat images to analyse the spatial distribution of the lineament and their geometric patterns for avialable information.Combined with geological,geophydical and seismological data,a further investigation is made for the main characteristics of the acnvitity of blocks and their boundary faults in the plateau and their generations.