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《GEOTECTONICA ET METALLOGENIA》 2000-02
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THE MECHANISM OF THE DIFFERENCE BETWEEN THENORTHERN PART AND THE SOUTHERN PART OFTHE FOLD AND THRUST BELT ON THE WESTERNEDGE OF THE ORDOS BASIN,CHINA

ZHANG Jin, MA Zong-jin,REN Wen-jun(1.Institute of Geology,CSB,Beijing 100029, China)(2.Department of Earth Sciences,Nanjing university,Nanjing 210093, China)  
The western fold and thrust belt of the Ordos basin is an important intracontinental thrust belt in China.It is a transfer zone between the west tectonic domain and the east tectonic domain of China, and also a good region for studying the lateral extension of the Qinghai-Tibet plateau,So it is important to understand its development and history.By discussing several questions about this belt and some areas near it,we make a hypothesis that it was the rotation in that time that led to the development of the belt.The belt can be divided into two parts by the Jintaquan-Balunbieli fault.It was the northeastern compression of the Qilian Mountain-Northern Qinling Orogen that led to the formation of the southern part of the belt, whereas the formation of the northern part of the belt was due to the rotation of the Ordos basin and the eastward extrusion of the Alshan Block. So the mechanism of the two parts was different.And we bring forward some views about several other questions.
【Fund】: 国家自然科学基金!(49834020)资助
【CateGory Index】: P542
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