Mesozoic extensional structures of the Fangshan tectonic dome and their subsequent reworking during collisional accretion of the North China Block
- 1 January 2006
- journal article
- Published by Geological Society of London in Journal of the Geological Society
- Vol. 163 (1), 127-142
- https://doi.org/10.1144/0016-764904-154
Abstract
The Fangshan area, SW of Beijing, lies at the junction of the NNE-trending Taihang mountain range and the southeastern portion of the Yanshan intraplate orogenic belt and has undergone at least five stages of deformation. Mid- to late Triassic extensional deformation (D1) is represented by the formation of the Fangshan tectonic dome during SE-directed extensional tectonics. This deformation was later modified by NNW-directed thrusting in the late Triassic (D2) and WNW-directed thrusting in the late Jurassic (D3). These D1-D3 structures were deformed by the arcuate Beiling syncline (D4), which formed during the intrusion of the 133-128 Ma Fangshan pluton. D5 deformation is represented by Cretaceous to Quaternary NNE-striking high-angle normal faults. The ages of these events demonstrate that the principal ENE-trending tectonic framework of the Yanshan intraplate orogenic belt was established mainly in the mid- to late Triassic (the Indosinian event). The Jurassic to Cretaceous Yanshanian deformation with thick-skinned thrusting was associated with intrusion of numerous plutons, and strongly modified the older structures. The tectonic evolution of the Fangshan tectonic dome was linked genetically with the collision of the North China Block and the Siberian Craton, and the later collision of the North and South China blocks.link_to_subscribed_fulltexKeywords
This publication has 38 references indexed in Scilit:
- A new geodynamic interpretation for the South Portuguese Zone (SW Iberia) and the Iberian Pyrite Belt genesisTectonics, 2003
- What drove late Mesozoic extension of the northern China–Mongolia tract?Tectonophysics, 2003
- Origin and tectonic significance of a Mesozoic multi-layer over-thrust system within the Yangtze Block (South China)Tectonophysics, 2002
- Late Mesozoic and Cenozoic rifting and its dynamic setting in Eastern China and adjacent areasTectonophysics, 2001
- Origin of the Uinta recess, Sevier fold–thrust belt, Utah: influence of basin architecture on fold–thrust belt geometryTectonophysics, 1999
- Geodynamics of the western part of the Mongolia–Okhotsk collisional belt, Trans-Baikal region (Russia) and MongoliaTectonophysics, 1999
- Geometric and kinematic evolution of basement-cored structures: intraplate orogenesis within the Yanshan Orogen, northern ChinaTectonophysics, 1998
- North and South China collision along the eastern and southern North China marginsTectonophysics, 1997
- The geodynamic evolution of the eastern Eurasian margin in Mesozoic timesTectonophysics, 1992
- New paleomagnetic results from northern China: collision and suturing with Siberia and KazakhstanTectonophysics, 1990