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EARLY TRIASSIC PALEOMAGNETIC RESULTS FROM SOUTHERN PART OF THE SICHUAN BASIN AND ITS TECTONIC IMPLICATIONS

Yang Zhenyu (Institute of Geomechanics, Chinese Academy of Geological Sciences Beijing\ 100081) Jean Besse (Institut de Physique du Globe de Paris, France 75252 Paris Cedex 05)  
Early Triassic paleomagnetic results from southern part of Sichuan basin indicate that a series of fold belt zones distributed in the east and southeast of the Sichuan province were not resulted from the oroclinal (rotation) bending. It was probably caused by the thrusting associated with deep-seated faulting. A comparison with the Triassic paleomagnetic results from the North China block (NCB) suggested that the final amalgamation between the NCB and the Yangzi block was post-Early Triassic, propably Early/Middle Jurassic.
【Fund】: 地质矿产部地质力学研究所地质力学开放实验室资助
【CateGory Index】: P542
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