ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
青藏高原北缘断裂擦痕的构造分析
  
关键词:northern Tibet Qinghai plateau  tectonic stress field  fault slip  computer processing
基金项目:地矿部深部项目
作者单位
李有社 中国地质科学院岩石圈中心 
崔军文 中国地质科学院岩石圈中心 
高静 中国地质科学院岩石圈中心 
唐哲明 中国地质科学院岩石圈中心 
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摘要:
A Study on Tectonic Stress's Field of Brittle Deformation in the Northern Tibet Qinghai Plateau
      Through field observation and computer processing of fault slip data, we divided the brittle tectonic stress' fields in the northern Tibet Qinghai plateau into two periods: Oligocene middle Pleistocene and middle Pleistocene Holocene. The maximum principal stress's orientation is approximately S N direction in the former period and N E in Altyn Taph and N W in Qilian respectively in the latter one. Meanwhile, geodyncmics of the northern Tibet Qinghai plateau is analysized.
LI You-she,CUI Jun-wen,GAO Jing,TANG Zhe-ming.1997.A Study on Tectonic Stress's Field of Brittle Deformation in the Northern Tibet Qinghai Plateau[J].Acta Geoscientica Sinica,18(2):129-133.
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