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青藏高原东北缘最新构造变形的初步研究
引用本文:戴华光,贾云鸿,苏向洲,陈永明,刘洪春,侯康明. 青藏高原东北缘最新构造变形的初步研究[J]. 地质力学学报, 1996, 2(4): 15-20
作者姓名:戴华光  贾云鸿  苏向洲  陈永明  刘洪春  侯康明
作者单位:国家地震局兰州地震研究所
摘    要:
在分析研究青藏高原东北缘地震、地震形变带及活动断裂带的基础上,确定了NNW向最新活动构造体系。该体系的主体构造是由一系列呈NNW向相间展布的现代隆起带和沉降带组成。青藏高原东北缘最新构造变形是该构造体系活动的结果。另外,还对体系的变形特征及"敏感点"进行了较详细的探讨。 

关 键 词:地震形变带   活动断裂   活动构造体系   最新构造变形

PRELIMINARY STUDY ON THE LATEST TECTONIC DEFORMATIONS ALONG NORTHEAST MARGIN OF THE QINGHAI-TIBETAN PLATEAU
Dai Huaguang,Jia Yunhong,Su Xiangzhou,Chen Yongming,Liu Hongchun and Hou Kangming. PRELIMINARY STUDY ON THE LATEST TECTONIC DEFORMATIONS ALONG NORTHEAST MARGIN OF THE QINGHAI-TIBETAN PLATEAU[J]. Journal of Geomechanics, 1996, 2(4): 15-20
Authors:Dai Huaguang  Jia Yunhong  Su Xiangzhou  Chen Yongming  Liu Hongchun  Hou Kangming
Affiliation:Earthquake Research Institute of Lanzhou, SSB
Abstract:
A recently active tectonic system which strikes NNW is determined by analyzing and Studying the earthquakes, seismic deformation bands and active fault zones along the northeastern margin of the Qinghai-Tibetan Plateau. It consists mainly of a series of modern uplifts alternating with sudsidence zones. The latest tectonic deformation along the north-eastern margin of the plateau was found to have resulted from the activity of the system. In addition, a more detailed discussion of the deformation of the system and the earthquake-prone areas is made.
Keywords:seismic deformation hands  active fault  active tectonic system  recently tectonic formation
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