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Reconstructing South China in Phanerozoic and Precambrian supercontinents

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Reconstructing South China in Phanerozoic and Precambrian supercontinents. / Cawood, Peter A.; Zhao, Guochun; Yao, Jinlong; Wang, Wei; Xu, Yajun; Wang, Yuejun.

In: Earth Science Reviews, Vol. 186, 11.2018, p. 173-194.

Research output: Contribution to journalArticle

Harvard

Cawood, PA, Zhao, G, Yao, J, Wang, W, Xu, Y & Wang, Y 2018, 'Reconstructing South China in Phanerozoic and Precambrian supercontinents', Earth Science Reviews, vol. 186, pp. 173-194. https://doi.org/10.1016/j.earscirev.2017.06.001

APA

Cawood, P. A., Zhao, G., Yao, J., Wang, W., Xu, Y., & Wang, Y. (2018). Reconstructing South China in Phanerozoic and Precambrian supercontinents. Earth Science Reviews, 186, 173-194. https://doi.org/10.1016/j.earscirev.2017.06.001

Vancouver

Cawood PA, Zhao G, Yao J, Wang W, Xu Y, Wang Y. Reconstructing South China in Phanerozoic and Precambrian supercontinents. Earth Science Reviews. 2018 Nov;186:173-194. https://doi.org/10.1016/j.earscirev.2017.06.001

Author

Cawood, Peter A. ; Zhao, Guochun ; Yao, Jinlong ; Wang, Wei ; Xu, Yajun ; Wang, Yuejun. / Reconstructing South China in Phanerozoic and Precambrian supercontinents. In: Earth Science Reviews. 2018 ; Vol. 186. pp. 173-194.

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@article{7a6d21085d4f41c28563df9fa577eed2,
title = "Reconstructing South China in Phanerozoic and Precambrian supercontinents",
abstract = "The history of the South China Craton and the constituent Yangtze and Cathaysia blocks are directly linked to Earth's Phanerozoic and Precambrian record of supercontinent assembly and dispersal. Exposed Archean rocks are limited to isolated fragments in the Yangtze Block that preserve a record of Meso- to Neo-Archean magmatism, sedimentation and metamorphism associated with a period of global craton formation and stabilization that corresponds with the assembly of the Kenor supercontinent/supercraton. However, there are insufficient data to link its history with other similar aged cratons. The tectonostratigraphic record in South China in the Paleoproterozoic, corresponding with the assembly of Nuna, suggests that rock units in the Yangtze Block were spatially linked with northwestern Laurentia and possibly Siberia, whereas Cathaysia was joined to northern India. During the formation of Rodinia at the end of the Mesoproterozoic through to that of Pangea in the mid-Paleozoic, Cathaysia remained joined to northern India. Early Neoproterozoic supra-subduction zone magmatic arc-back arc assemblages ranging in age from ~ 1000 Ma to 810 Ma occur within Cathaysia, along its northwestern margin, and along the southeastern margin of the Yangtze Block. These rocks provide a record of convergent plate interaction, which continued along the western margin of the Yangtze Block until around 700 Ma and correlates with similar along strike subduction zone magmatism in northwest India, Seychelles and Madagascar. During the final assembly of Gondwana in the early Paleozoic suturing of India-South China with the Western Australia-Mawson blocks along the Kuunga Orogen resulted in the accretion of the Sanya Block of Hainan Island with the rest of Cathaysia. The accretion of Laurussia to Gondwana in the mid-Paleozoic to form Pangea corresponds with the initiation of lithospheric extension along the northern margin of Gondwana and the separation of a number of continental blocks, including South China, which then drifted northward across the Paleo-Tethys to collide with the Asian segment of Pangea in the Permo-Triassic.",
keywords = "Supercontinent, Pangea, Gondwana, Rodinia, Nuna",
author = "Cawood, {Peter A.} and Guochun Zhao and Jinlong Yao and Wei Wang and Yajun Xu and Yuejun Wang",
note = "This paper is financially supported by a NSFC Major Program (41190070) entitled “Reconstruction of East Asian Blocks in Pangea”. PAC acknowledges support from the Australian Research Council grant FL160100168 and WW thanks the support from “Thousand Youth Talents Plan”.",
year = "2018",
month = "11",
doi = "10.1016/j.earscirev.2017.06.001",
language = "English",
volume = "186",
pages = "173--194",
journal = "Earth Science Reviews",
issn = "0012-8252",
publisher = "Elsevier Science BV",

}

RIS (suitable for import to EndNote) - Download

TY - JOUR

T1 - Reconstructing South China in Phanerozoic and Precambrian supercontinents

AU - Cawood, Peter A.

AU - Zhao, Guochun

AU - Yao, Jinlong

AU - Wang, Wei

AU - Xu, Yajun

AU - Wang, Yuejun

N1 - This paper is financially supported by a NSFC Major Program (41190070) entitled “Reconstruction of East Asian Blocks in Pangea”. PAC acknowledges support from the Australian Research Council grant FL160100168 and WW thanks the support from “Thousand Youth Talents Plan”.

PY - 2018/11

Y1 - 2018/11

N2 - The history of the South China Craton and the constituent Yangtze and Cathaysia blocks are directly linked to Earth's Phanerozoic and Precambrian record of supercontinent assembly and dispersal. Exposed Archean rocks are limited to isolated fragments in the Yangtze Block that preserve a record of Meso- to Neo-Archean magmatism, sedimentation and metamorphism associated with a period of global craton formation and stabilization that corresponds with the assembly of the Kenor supercontinent/supercraton. However, there are insufficient data to link its history with other similar aged cratons. The tectonostratigraphic record in South China in the Paleoproterozoic, corresponding with the assembly of Nuna, suggests that rock units in the Yangtze Block were spatially linked with northwestern Laurentia and possibly Siberia, whereas Cathaysia was joined to northern India. During the formation of Rodinia at the end of the Mesoproterozoic through to that of Pangea in the mid-Paleozoic, Cathaysia remained joined to northern India. Early Neoproterozoic supra-subduction zone magmatic arc-back arc assemblages ranging in age from ~ 1000 Ma to 810 Ma occur within Cathaysia, along its northwestern margin, and along the southeastern margin of the Yangtze Block. These rocks provide a record of convergent plate interaction, which continued along the western margin of the Yangtze Block until around 700 Ma and correlates with similar along strike subduction zone magmatism in northwest India, Seychelles and Madagascar. During the final assembly of Gondwana in the early Paleozoic suturing of India-South China with the Western Australia-Mawson blocks along the Kuunga Orogen resulted in the accretion of the Sanya Block of Hainan Island with the rest of Cathaysia. The accretion of Laurussia to Gondwana in the mid-Paleozoic to form Pangea corresponds with the initiation of lithospheric extension along the northern margin of Gondwana and the separation of a number of continental blocks, including South China, which then drifted northward across the Paleo-Tethys to collide with the Asian segment of Pangea in the Permo-Triassic.

AB - The history of the South China Craton and the constituent Yangtze and Cathaysia blocks are directly linked to Earth's Phanerozoic and Precambrian record of supercontinent assembly and dispersal. Exposed Archean rocks are limited to isolated fragments in the Yangtze Block that preserve a record of Meso- to Neo-Archean magmatism, sedimentation and metamorphism associated with a period of global craton formation and stabilization that corresponds with the assembly of the Kenor supercontinent/supercraton. However, there are insufficient data to link its history with other similar aged cratons. The tectonostratigraphic record in South China in the Paleoproterozoic, corresponding with the assembly of Nuna, suggests that rock units in the Yangtze Block were spatially linked with northwestern Laurentia and possibly Siberia, whereas Cathaysia was joined to northern India. During the formation of Rodinia at the end of the Mesoproterozoic through to that of Pangea in the mid-Paleozoic, Cathaysia remained joined to northern India. Early Neoproterozoic supra-subduction zone magmatic arc-back arc assemblages ranging in age from ~ 1000 Ma to 810 Ma occur within Cathaysia, along its northwestern margin, and along the southeastern margin of the Yangtze Block. These rocks provide a record of convergent plate interaction, which continued along the western margin of the Yangtze Block until around 700 Ma and correlates with similar along strike subduction zone magmatism in northwest India, Seychelles and Madagascar. During the final assembly of Gondwana in the early Paleozoic suturing of India-South China with the Western Australia-Mawson blocks along the Kuunga Orogen resulted in the accretion of the Sanya Block of Hainan Island with the rest of Cathaysia. The accretion of Laurussia to Gondwana in the mid-Paleozoic to form Pangea corresponds with the initiation of lithospheric extension along the northern margin of Gondwana and the separation of a number of continental blocks, including South China, which then drifted northward across the Paleo-Tethys to collide with the Asian segment of Pangea in the Permo-Triassic.

KW - Supercontinent

KW - Pangea

KW - Gondwana

KW - Rodinia

KW - Nuna

U2 - 10.1016/j.earscirev.2017.06.001

DO - 10.1016/j.earscirev.2017.06.001

M3 - Article

VL - 186

SP - 173

EP - 194

JO - Earth Science Reviews

JF - Earth Science Reviews

SN - 0012-8252

ER -

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