DOI: 10.1016/j.earscirev.2020.103357
论文题名: Mesozoic-Cenozoic basin inversion and geodynamics in East China: A review
作者: Suo Y. ; Li S. ; Cao X. ; Wang X. ; Somerville I. ; Wang G. ; Wang P. ; Liu B.
刊名: Earth Science Reviews
ISSN: 00128252
出版年: 2020
卷: 210 语种: 英语
中文关键词: Basin inversion
; Dynamic topography
; East China
; Eastward migration
; Northward migration
; Okhotomorsk Block
英文关键词: basin evolution
; Cenozoic
; diachronism
; fission track dating
; geodynamics
; Mesozoic
; oceanic crust
; Pacific plate
; plate tectonics
; tectonic evolution
; tectonic setting
; uplift
; China
英文摘要: East China experienced alternating tectonic extension and compression with ambiguous tectonic settings in the Mesozoic-Cenozoic interval. Long-term extensional episodes associated with the subduction retreat of the Paleo-Pacific and Pacific slabs have been widely studied. The compressional events, of which basin inversion is a typical case, are less concerned, but important in understanding the tectonic evolution and geodynamics in East China. We made a systematic study, involving tectonics, sedimentation, apatite fission track, and dynamic topography, on the Mesozoic-Cenozoic basin inversion in East China. Four-phases of basin inversion were concluded: (1) Early-Late Cretaceous inversion occurred at 115-100 Ma in Southeast China and at 100-89 Ma in Northeast China, showing a northward migration due to the diachronous collision of the northward moving Okhotomorsk Block with East Asia. (2) The latest Cretaceous-Early Paleogene inversion was widely developed throughout East China. It is associated with the increasingly younger subducted oceanic crust of the Izanagi Plate, which caused the progressively increasing buoyancy beneath East China and an uplift in dynamic topography. Cenozoic inversion showed an eastward migration, from (3) the western part of each basin at the Late Paleogene to (4) the eastern part at the Neogene, due to the subduction retreat of the Pacific Plate. © 2020 Elsevier B.V. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/166267
Appears in Collections: 气候变化与战略
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作者单位: Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao, 266100, China; Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao, 266100, China; UCD School of Earth Sciences, University College Dublin, Belfield, Dublin 4, Ireland
Recommended Citation:
Suo Y.,Li S.,Cao X.,et al. Mesozoic-Cenozoic basin inversion and geodynamics in East China: A review[J]. Earth Science Reviews,2020-01-01,210