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Terra Nova 24, 6 (2012) 456-466
Is the Jurassic (Yanshanian) intraplate tectonics of North China due to westward indentation of the North China block?
Michel Faure 1, Wei Lin 2, Yan Chen 1
(2012)

The northern mountains of Beijing are the type locality of the Mesozoic Yanshanian orogen. Our structural study emphasizes the importance of dextral strike-slip for the formation of this intracontinental belt. The South- and North-directed thrusts are positive flower structures rooted in strike-slip faults. This transpressional tectonics developed from Late Triassic to Late Jurassic-Early Cretaceous through three deformation phases coeval with syntectonic sedimentation, separated by two transtensional episodes coeval with magmatism. The Late Jurassic-Early Cretaceous tectonic event is also recognized in several places of North China. Strike-slip faulting controls the deformation of the northern border of the North China block in the Yanshan-Yinshan belt. Simultaneously, East-directed thrusts and folds develop along N-S elongated ranges in Helanshan, Shanxi highlands and Taihangshan. The Jurassic tectonics of the North China Block is interpreted in a unitary way as the result of the westward underthrusting of the North China block below the Alashan block.
1 :  Institut des Sciences de la Terre d'Orléans (ISTO)
Université d'Orléans – CNRS : UMR7327 – INSU – Bureau de Recherches Géologiques et Minières (BRGM)
2 :  State Key Laboratory of Lithospheric Evolution
Institute of Geology and Geophysics, Chinese Academy of Sciences
Planète et Univers/Sciences de la Terre/Tectonique

Sciences de l'environnement/Milieux et Changements globaux
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