globalchange  > 影响、适应和脆弱性
DOI: 10.1016/j.epsl.2018.03.057
Scopus记录号: 2-s2.0-85045034938
论文题名:
Cenozoic lithospheric deformation in Northeast Asia and the rapidly-aging Pacific Plate
作者: Yang T.; Moresi L.; Zhao D.; Sandiford D.; Whittaker J.
刊名: Earth and Planetary Science Letters
ISSN: 0012821X
出版年: 2018
卷: 492
起始页码: 1
结束页码: 11
语种: 英语
英文关键词: Baikal Rift Zone ; Japan Sea ; Northeast Asia ; stagnant slab ; subduction ; tectonics
Scopus关键词: Geodynamics ; Metamorphic rocks ; Baikal rift zone ; Japan Sea ; Northeast Asia ; Stagnant slabs ; subduction ; Tectonics ; Cenozoic ; continental lithosphere ; deformation ; geodynamics ; magmatism ; Oligocene ; Pacific plate ; rifting ; seafloor spreading ; slab ; spatiotemporal analysis ; subduction zone ; trench ; Asia ; Baikal Rift Zone ; Pacific Ocean ; Russian Federation ; Sea of Japan
英文摘要: Northeast Asia underwent widespread rifting and magmatic events during the Cenozoic. The geodynamic origins of these tectonic events are often linked to Pacific plate subduction beneath Northeast Asia. However, the Japan Sea did not open until the late Oligocene, tens of millions of years after Pacific Plate subduction initiation in the Paleocene. Moreover, it is still not clear why the Baikal Rift Zone extension rate increased significantly after the late Miocene, while the Japan Sea opening ceased at the same time. Geodynamic models suggest these enigmatic events are related to the rapidly-aging Pacific Plate at the trench after Izanagi–Pacific spreading ridge subduction. Subduction of the young Pacific Plate delayed the Japan Sea opening during the Eocene while advection of the old Pacific Plate towards the trench increases seafloor age rapidly, allowing the Japan Sea to open after the early Miocene. The Japan Sea opening promotes fast trench retreat and slab stagnation, with subduction-induced wedge zone convection gradually increasing its extent during this process. The active rifting center associated with wedge zone convection upwelling also shifts inland-ward during slab stagnation, preventing further Japan Sea spreading while promoting the Baikal Rift Zone extension. Our geodynamic model provides a good explanation for the temporal-spatial patterns of the Cenozoic tectonic and magmatic events in Northeast Asia. © 2018 Elsevier B.V.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/109901
Appears in Collections:影响、适应和脆弱性
气候变化事实与影响

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作者单位: School of Earth Sciences, University of Melbourne, Melbourne, VIC 3000, Australia; Department of Geophysics, Tohoku University, Sendai, 980-8578, Japan; Institute for Marine and Antarctic Studies, University of Tasmania, Hobart, Tasmania 7001, Australia

Recommended Citation:
Yang T.,Moresi L.,Zhao D.,et al. Cenozoic lithospheric deformation in Northeast Asia and the rapidly-aging Pacific Plate[J]. Earth and Planetary Science Letters,2018-01-01,492
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