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《GEOTECTONICA ET METALLOGENIA》 2000-03
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RELATIONSHIP BETWEEN THE WRENCH STRUCTURE IN THE NORTH- MARGIN BLOCK- FAULTING BELT IN THE QAIDAM BASIN AND ALTUN TECTONIC SYSTEM

ZHANG Shou- ren1, CAO Dai- yong1, DAI Jun- sheng2, LI Jian- hong3 (1.China University of Mining and Technology,Beijing 100083,China) (2 University of Petroleum, Dongying 257004,Shandong, China) (3 Daqing Donghua Group, Daqing 163000,Heilongjiang, Ch  
From the aspects of the change of structural line orientation and the non- coincide of the deep and shallow structure features,the left- handed echelon and the reverse “ S” structure assembles,and the move of Mesozoic group from old to new from west to east in the north- margin block- faulting belt in the the Qaidam Basin,this paper demonstrates in detail the ideas,that the north- margin block- faulting belt in the Qaidam Basin is shaped under the control of Qiulitage tectonic system and the reconstruction of Altun tectonic system,that the recent structural pattern in the north- margin block- faulting belt in the Qaidam Basin has resulted from the effect of Altun tectonic system. And on the basis of these ideas, this paper summarizes the characteristics of structural development in the north- margin block- faulting belt in the Qaidam Basin.
【Fund】: 石油天然气总公司“九五”科技攻关项目!(项目号:970208)的部分研究成果.
【CateGory Index】: P552
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