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《Acta Scientiarum Naturalium Universitatis Pekinensis》 2012-01
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Geometric and Tectonophysical Simulate of the Bachu Fold Belt:Central Region of Tarim Basin

ZHANG Bo1,YAN Shuyu1,ZHANG Zhongpei2,ZHANG Jinjiang1,ZHENG Yadong1,WANG Xiaoxian1,WANG Meng1,WANG Jiamin1 1.The Key Laboratory of Orogenic Belts and Crustal Evolution(MOE),School of Earth and Space Sciences,Peking University,Beijing 100871;2.SINOPEC Exploration and Production Research Institute,Beijing 100083  
Based on structural geometries,kinematic observations,and sand-box simulation results,the new interpretation explains that the Bachu fold belt in the Tarim basin is composed of detachment folds flanked by various-scale kink bands primarily unassociated with faulting.The Bachu antiform belt is characterized by the detachment fold.The detachment fold crests are bounded by kink bands,which are narrow zones of angularly folded strata.The substantial width of these kink bands,their sub-parallel edges in the outcrop cross-sections,and their orientation at a high angle to layering,as well as their organized spacing and conjugate geometry,support a kink-band interpretation.Application of sandbox models for tectonic simulate modeling regenerates kink-band development and evolution:wide-gentle detachment folding → tight detachment folding → fold pop-up → fault adjusting.The analog results strongly support that the kink-band is one of the structure types to form the Bachu fold zone.
【Fund】: 国家自然科学基金(40802050);; 中国石油化工股份有限公司科技攻关项目资助
【CateGory Index】: P542.2
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