4.5 Article

Early Cretaceous extensional reworking of the Triassic HP-UHP metamorphic orogen in Eastern China

期刊

TECTONOPHYSICS
卷 662, 期 -, 页码 256-270

出版社

ELSEVIER
DOI: 10.1016/j.tecto.2015.05.028

关键词

Early Cretaceous extensional tectonics; Superimposed orogens; Trassic HP-UHP orogenic belt; Tongbai-Dabie-Sulu; Eastern China

资金

  1. NSFC [41225009, 41472193]
  2. Project of Major State Special Research on Petroleum [2011ZX05008-001]
  3. Strategic Priority Research Program of the Chinese Academy of Science [XDB03020203]

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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 1000 km-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. (C) 2015 Elsevier B.V. All rights reserved.

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