Volume 27 Issue 5
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LIU Xiaochun, ZHAO Yue, WANG Wei, et al., 2021. Ancient cratonic nuclei in East Antarctica: Research status, problems and prospects. Journal of Geomechanics, 27 (5): 691-704. DOI: 10.12090/j.issn.1006-6616.2021.27.05.057
Citation: LIU Xiaochun, ZHAO Yue, WANG Wei, et al., 2021. Ancient cratonic nuclei in East Antarctica: Research status, problems and prospects. Journal of Geomechanics, 27 (5): 691-704. DOI: 10.12090/j.issn.1006-6616.2021.27.05.057
shu

Ancient cratonic nuclei in East Antarctica: Research status, problems and prospects

doi: 10.12090/j.issn.1006-6616.2021.27.05.057
  • 1.

    Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

  • 2.

    Research Center for Polar Geosciences, China Geological Survey, Beijing 100081, China

  • 3.

    Key Laboratory of Paleomagnetism and Tectonic Reconstruction of Ministry of Natural Rescources, Beijing 100081, China

  • 4.

    Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

Funds:

the National Natural Sciences Foundation of China 41941004

More Information
  • Received: 2021-07-09
  • Revised: 2021-08-28
    • Available Online: 2021-12-31
  • Published: 2021-10-28
    Abstract
  • The Archean cratonic nuclei in the East Antarctic Shield (Craton) occur mainly in the Napier Mountains, southern Prince Charles Mountains, Rauer Group and Vestfold Hills in the Indian Ocean sector, and are sporadically exposed in the Australian, African and Pacific sectors. These ancient nuclei with diverse earlier crustal histories and later reworking processes are separated by the Paleoproterozoic-Early Paleozoic (Pan-African-aged) orogens. The nuclei in different sectors have a close affinity with the adjacent Gondwana continental blocks. Integrated bedrock and subglacial geological investigations and petrological and chemical studies will ascertain the temporal and spatial distributions, petrogenesis, source regions, tectonic affinities and multiple metamorphic records of the Archean rocks (materials) in East Antarctica.This can help to reveal the major history from nucleation to assembly of the East Antarctica continent, and thus to contribute to a better understanding of the early history of the Earth from an Antarctic perspective.

     

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