断层相关褶皱理论与应用研究新进展.pdfVIP

第 12 卷第4 期 地学前缘( 中国地质大学( 北京); 北京大学) Vol. 12 No. 4 2005 年 10 月 Earth Science Frontiers (China University of Geosciences, Beijing; eking University) Oct. 2005 断层相关褶皱理论与应用研究新进展 1, 2 2 1 何登发 , John SU E , 贾承造 11 中国石油勘探开发研究院, 北京 100083 21 美国普林斯顿大学 地球科学系, 新泽西州 08544 1, 2 2 1 HE Deng2fa , John SU E , JIA Cheng2zao 11 Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China 21 Department of Geosciences, Princeton University, ewJ ersey 08544, USA HE Den g2 fa, SUPP E J , JIA Chen g2 zao. New a dvan ces in th eory an d app ication of fau t2re at ed fo ding. E ar th Scien ce F r on2 t ier s, 2005, 12 ( 4) : 3532 364 Abstr act : Rich introduced the geometry of fault2bend fold of the Appalachian Mountains in 1934. H alf a centu2 ry later, Suppe first quantified it, and established relationships between fold geometry, fault geometry and fault slip that led to the foundation of the theory of fault2 related folding. Since then, much of progress has been made not only in establishing the geometric and kinemat ic models of the end2members such as fault2propa2 gation folding and fault2 detachment folding, but also in putting forward a series of superimposed models of fault2related folds such as imbricate structures, tectonic wedges, and interference structures, et c. . Concerning syntect onic sedimentation, growth fault2related folding theory was set forth giving a quantit ative represent ation between sedimentation and the fault2 slip rate, folding rate, and uplifting rate. As far as the mechanical strat ig2 raphy and deformat ion character are concerned, the shear fault2bend folding is put forward. A series of me2 chanical models are est ablished as being well base