Journal articles
Early Cretaceous extensional reworking of the Triassic HP-UHP metamorphic orogen in Eastern China
Abstract : Corresponding to the Early Mesozoic continental subduction between the North China Block (NCB) and the South China Block (SCB), the Tongbaishan-Hong’an- Dabieshan-Sulu massifs are famous for their HP-UHP metamorphism. More than 50% of the HP-UHP Orogenic Belt was significantly reworked by Early Cretaceous extensional tectonics. This Early Cretaceous event with a fast cooling period, at 130-120 Ma, superimposed on the Early Mesozoic HP-UHP orogenic belt and intensively changed the architecture of this orogen. Each individual segment documents different Early Cretaceous extensional structures, namely the central Tongbaishan domain is a metamorphic core complex (MCC) represented by an A-type non-cylindrical antiform; the central Dabieshan domain is a typical Cordilleran-type migmatite-cored MCC; the Southern Sulu UHP domain is a “wedge-shaped” structure exhumed by a simple detachment fault. These late stage extensional structures expose the previous HP-UHP orogenic belt as fragments along the NCB-SCB boundary. The geodynamic setting of this Early Cretaceous extensional tectonics along the HP-UHP orogen is a part of a 1000km-scale crustal extension belt that is widespread in eastern Eurasia continent from Trans-Baikal to the central part of SCB. Convective erosion or delamination of the mantle lithosphere might be considered as a possible mechanism for mantle removal.
Cited literature [59 references]
https://hal-insu.archives-ouvertes.fr/insu-01167486
Contributor : Nathalie Pothier <>
Submitted on : Wednesday, June 24, 2015 - 4:08:35 PM
Last modification on : Wednesday, October 14, 2020 - 4:07:47 AM
Long-term archiving on: : Tuesday, April 25, 2017 - 6:09:21 PM
Contributor : Nathalie Pothier <>
Submitted on : Wednesday, June 24, 2015 - 4:08:35 PM
Last modification on : Wednesday, October 14, 2020 - 4:07:47 AM
Long-term archiving on: : Tuesday, April 25, 2017 - 6:09:21 PM
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