Origin and tectonic significance of a Mesozoic multi-layer over-thrust system within the Yangtze Block (South China) Dan-Ping Yan a,b,c , Mei-Fu Zhou b, * , Hong-Lin Song a , Xin-Wen Wang a , John Malpas b a School of Earth Sciences and Resources, China University of Geosciences, Beijing, China b Department of Earth Sciences, The University of Hong Kong, Pokfulam Road, Hong Kong SAR, China c The Key Laboratory of Lithospheric Tectonics and Exploration, China University of Geosciences, Ministry of Education, Beijing, China Received 28 May 2002; accepted 31 October 2002 Abstract In the Yangtze Block (South China), a well-developed Mesozoic thrust system extends through the Xuefeng and Wuling mountains in the southeast to the Sichuan basin in the northwest. The system comprises both thin- and thick-skinned thrust units separated by a boundary detachment fault, the Dayin fault. To the northwest, the thin-skinned belt is characterized by either chevron anticlines and box synclines to the northwest or chevron synclines to the southeast. The former structural style displays narrow exposures for the cores of anticlines and wider exposures for the cores of synclines. Thrust detachments occur along Silurian (Fs) and Lower Cambrian (Fc) strata and are dominantly associated with the anticlines. To the southeast, this style of deformation passes gradually into one characterized by chevron synclines with associated principal detachment faults along Silurian (Fs), Cambrian (Fc) and Lower Sinian (Fz) strata. There are, however, numerous secondary back thrusts. Therefore, the thin-skinned belt is like the Valley and Ridge Province of the North American Applachian Mountains. The thick-skinned belt structurally overlies the thin-skinned belt and is characterized by a number of klippen including the Xuefeng and Wuling nappes. It is thus comparable to the Blue Ridge Province of Appalachia. The structural pattern of this thrust system in South China can be explained by a model involving detachment faulting along various stratigraphic layers at different stages of its evolution. The system was developed through a northwest stepwise progression of deformation with the earliest delamination along Lower Sinian strata (Fz). Analyses of balanced geological cross-sections yield about 18.1 – 21% (total 88 km) shortening for the thin-skinned unit and at least this amount of shortening for the thick-skinned unit. The compressional deformation from southeast to northwest during Late Jurassic to Cretaceous time occurred after the westward progressive collision of the Yangtze Block with the North China Block and suggests that the orogenic event was intracontinental in nature. D 2002 Elsevier Science B.V. All rights reserved. Keywords: Balanced geological section; Thrust fault; Thin- and thick-skinned structure; Nappe; Intracontinental event; Yangtze Block of China 1. Introduction Large scale Mesozoic deformation in South China (Fig. 1), which is in many ways similar to the Valley and Ridge tectonic system of the Appalachian Moun- 0040-1951/02/$ - see front matter D 2002 Elsevier Science B.V. All rights reserved. doi:10.1016/S0040-1951(02)00646-7 * Corresponding author. Tel.: +86-2857-8251; fax: +86-2517- 6912. E-mail address: mfzhou@hkucc.hku.hk (M.-F. Zhou). www.elsevier.com/locate/tecto Tectonophysics 361 (2003) 239– 254