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Research ArticleArticles

From Rodinia to Gondwanaland: A tale of detrital zircon provenance analyses from the southern Nanhua Basin, South China

Wei-Hua Yao, Zheng-Xiang Li, Wu-Xian Li, Xian-Hua Li and Jin-Hui Yang
American Journal of Science January 2014, 314 (1) 278-313; DOI: https://doi.org/10.2475/01.2014.08
Wei-Hua Yao
* ARC Center of Excellence for Core to Crust Fluid Systems (CCFS), The Institute for Geoscience Research (TIGeR), Department of Applied Geology, Curtin University, Perth, WA 6845, Australia
** Faculty of Earth Resource, China University of Geosciences, Wuhan 430074, China
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  • For correspondence: z.li@curtin.edu.au weihua.yao@postgrad.curtin.edu.au
Zheng-Xiang Li
* ARC Center of Excellence for Core to Crust Fluid Systems (CCFS), The Institute for Geoscience Research (TIGeR), Department of Applied Geology, Curtin University, Perth, WA 6845, Australia
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  • For correspondence: z.li@curtin.edu.au weihua.yao@postgrad.curtin.edu.au
Wu-Xian Li
*** Key Laboratory of Isotope Geochronology and Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
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Xian-Hua Li
§ State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
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Jin-Hui Yang
§ State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
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Abstract

The paleogeographic positions of the South China Block (SCB) during the Neoproterozoic and early Paleozoic are important for understanding the transition from the break-up of the supercontinent Rodinia to the formation of Gondwanaland. Integrated in situ U-Pb ages and Hf-O isotope analyses of detrital zircons from Cambrian sedimentary rocks in the southwestern SCB reveal major age populations at 2500 Ma, 1100 to 900 Ma, 850 to 750 Ma and 650 to 500 Ma, with a predominant group at ∼980 Ma that counts for ∼50 percent of all analyses. Zircon Hf-O isotopic results suggest three Precambrian episodes of juvenile crustal growth for the source area(s) (3.0 Ga, 2.5 Ga and 1.0 Ga), with major crustal reworking at 580 to 500 Ma. The source provenance as defined by the U-Pb and Hf analyses is distinctly different from the known tectonomagmatic record of the SCB, or that of western Australia or western Laurentia, but matches well with that of the Ediacaran (latest Neoproterozoic)–Cambrian clastic sedimentary rocks and granitic intrusions in the NW Indian Himalaya. The SCB–NW India provenance linkage appears to have started from the Ediacaran. We propose that after breaking away from central Rodinia, the SCB collided with NW India during the Ediacaran–Ordovician time, causing the “Pan-African” Kurgiakh/Bhimphedian orogeny at the northern margin of India as well as the intraplate Wuyi-Yunkai orogeny (>460 Ma − 415 Ma) in South China. The Ediacaran–lower Paleozoic clastic sedimentary rocks in the Nanhua Basin are therefore interpreted to be foreland deposits formed during the collision of the SCB with Gondwanaland.

  • Detrital zircon
  • Cambrian
  • Cathaysia Block
  • South China
  • North India
  • Rodinia
  • Gondwanaland
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American Journal of Science: 314 (1)
American Journal of Science
Vol. 314, Issue 1
1 Jan 2014
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From Rodinia to Gondwanaland: A tale of detrital zircon provenance analyses from the southern Nanhua Basin, South China
Wei-Hua Yao, Zheng-Xiang Li, Wu-Xian Li, Xian-Hua Li, Jin-Hui Yang
American Journal of Science Jan 2014, 314 (1) 278-313; DOI: 10.2475/01.2014.08

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From Rodinia to Gondwanaland: A tale of detrital zircon provenance analyses from the southern Nanhua Basin, South China
Wei-Hua Yao, Zheng-Xiang Li, Wu-Xian Li, Xian-Hua Li, Jin-Hui Yang
American Journal of Science Jan 2014, 314 (1) 278-313; DOI: 10.2475/01.2014.08
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Keywords

  • detrital zircon
  • Cambrian
  • Cathaysia Block
  • South China
  • North India
  • Rodinia
  • Gondwanaland

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