Plate convergence in the Indo-Pacific region

Weidong SUN; Lipeng ZHANG; Renqiang LIAO; Saijun SUN; Congying LI; He LIU

doi:10.1007/s00343-020-0146-y

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Plate convergence in the Indo-Pacific region

Review | Updated：2023-04-27

- Plate convergence in the Indo-Pacific region
- Plate convergence in the Indo-Pacific region
- 海洋湖沼学报（英文） 2020年38卷第4期
- Affiliations：
  
  1.Center of Deep Sea Research, Institute of Oceanology, Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China
  2.Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
  3.University of Chinese Academy of Sciences, Beijing 100049, China
- Author bio：
  
  SUN Weidong, weidongsun@qdio.ac.cn
- Funds：
  
  the Strategic Priority Research Program of the Chinese Academy of Sciences(XDB42020203);the Strategic Priority Research Program (B) of the Chinese Academy of Sciences(XDB18020102);National Key R & D Program of China(2016YFC0600408);the Taishan Scholar Program of Shandong(ts201712075);© Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag GmbH Germany, part of Springer Nature 2020
- DOI：10.1007/s00343-020-0146-y
  中图分类号：
- 收稿：2020-04-03，
  
  网络首发：2020-05-09，
  
  纸质出版：2020-07
- Accepted：
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Plate convergence in the Indo-Pacific region[J]. 海洋湖沼学报（英文）, 2020,38(4):1 017.

Weidong SUN, Lipeng ZHANG, Renqiang LIAO, et al. Plate convergence in the Indo-Pacific region[J]. Journal of Oceanology and Limnology, 2020, 38(4): 1 017.
Plate convergence in the Indo-Pacific region[J]. 海洋湖沼学报（英文）, 2020,38(4):1 017. DOI： 10.1007/s00343-020-0146-y.

Weidong SUN, Lipeng ZHANG, Renqiang LIAO, et al. Plate convergence in the Indo-Pacific region[J]. Journal of Oceanology and Limnology, 2020, 38(4): 1 017. DOI： 10.1007/s00343-020-0146-y.

摘要

Abstract

The Indo-Pacific convergence region is the best target to solve the two remaining challenges of the plate tectonics theory

i.e.

subduction initiation and the driving force of plate tectonics. Recent studies proposed that the Izu-Bonin subduction initiation belongs to spontaneous initiation

which implies that it started from extension

followed by low angle subduction. Numerical geodynamic modeling suggests that the initiation of plate subduction likely occurred along a transform fault

which put the young spreading ridge in direct contact with old oceanic crust. This

however

does not explain the simultaneous subduction initiation in the west Pacific region in the Cenozoic. Namely

the subduction initiations in the Izu-BoninMariana

the Aleutian

and the Tonga-Kermadec trenches are associated with oceanic crusts of different ages

yet they occurred at roughly the same time

suggesting that they were all triggered by a major change in the Pacific plate. Moreover

low angle subduction induces compression rather than extension

which requires external compression forces. Given that the famous Hawaiian-Emperor bending occurred roughly at the same time with the onset of westward subductions in the west Pacific

we propose that these Cenozoic subductions were initiated by the steering of the Pacific plate

which are classified as induced initiation. Induced subduction initiation usually occurs in young ocean basins

forming single-track subduction. The closures of Neo-Tethys Oceans were likely triggered by plumes in the south

forming northward subductions. Interestingly

the Indian plate kept on moving northward more than 50 Ma after the collision between the Indian and Eurasian continents and the break-off of the subducted oceanic slab attached to it. This strongly suggests that slab pull is not the main driving force of plate tectonics

whereas slab sliding is.

关键词

Keywords

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