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《Acta Scientiarum Naturalium Universitatis Pekinensis》 2008-03
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Structural Characteristics and Geological Significance of Karayulgun Fault in Northern Tarim Basin

HE Dian1, LI Jianghai 1,LI Baishou2 1Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871; 2Institute of Remote Sensing and GIS, Peking University, Beijing 100871;  
Karayulgun fault located in Northern Tarim Basin is one of northwest-trending faults of Northern Tarim Basin. Based on field investigation and interpretation of seismic profiles, it is found that Karayulgun fault is a right-lateral strike-slip fault accompanied with North-Ka, Mid-Ka, and South-Ka en echelon folds and secondary faults that are consistent with classical theoretical model of strike-slip fault. Karayulgun fault belt developed on the basis of NW-trending reverse faults in Paleozoic, which experienced compression in Paleozoic, calm sedimentation in Mesozoic, and compression and strike-slip movement in Cenozoic. The location between Wushi-Wensu and Kuqa-Tabei units makes the fault regulate the differential deformation of the two regions. The fault and associated structures provide a favorable condition for hydrocarbon migration and accumulation.
【Fund】: 国家自然科学基金资助项目(40242014)
【CateGory Index】: P542
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