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《EARTH SCIENCE FRONTIERS》 1999-03
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CONTRAST RESEARCH ON TIANSHAN OROGENIC BELT AND YINSHAN -YANSHAN OROGENIC BELT

Ma Zongjin; Zhao Junmeng(Institute of Geology, China Seismological Bureau, Beijing, 100029)  
Located at almost the same latitude, the Tianshan and the Yinshan - Yanshan are two important orogenic belts in northern China. The Tianshan orogenic belt within Chinese territory is situated in the northwestern China. It is also well known as a seismic zone. While the Yinshan - Yanshan orogenic belt is situated in the northeastern China. Small earthquakes have occurred scarcely in this belt, and no big one has taken place in the history which make this region a seismic blank area. The authors' research work shows that the differences in seis-micity are related to the tectonic environments. A compression envirorimnt exists in the north-western China and an extension environment in the northeastern China. As a Mesozoic and Cenozoic orogenic belt, the Tianshan orogenic belt exhibits a high tectonic activity at the mo-ment, while as a Proterozoic orogenic belt, the Yinshan - Yanshan orogenic belt has already passed its peak period of tectonic activity and only processes a lower level of tectonic activity at present. The development and occurrence of earthquakes are closely related to the deep struc-tures. The crust of the Tianshan orogenic belt develops the high conductivity layers and the correspondent lower velocity zones which make the crust to be very comlicated. In the Yin-shan- Yanshan orogenic belt, however, no high conductivity layers and lower velocity zone have been found there, so the crust structure is very simple. The existence of the high conduc-tivity layers and the lower velocity zones indicates that the tectonic activity is strong, which may provide a favourable condition for the development and occurrence of earthquakes.
【Fund】: 国家自然科学基金!49672166;;地震科学联合基金!196032
【CateGory Index】: P315
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