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    Volume 45 Issue 7
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    Article Navigation >  Earth Science  > 2020  >  45(7): 2245-2257
    Mo Xuanxue, 2020. Growth and Evolution of Crust of Tibetan Plateau from Perspective of Magmatic Rocks. Earth Science, 45(7): 2245-2257. doi: 10.3799/dqkx.2020.160
    Citation: Mo Xuanxue, 2020. Growth and Evolution of Crust of Tibetan Plateau from Perspective of Magmatic Rocks. Earth Science, 45(7): 2245-2257. doi: 10.3799/dqkx.2020.160
    shu

    Growth and Evolution of Crust of Tibetan Plateau from Perspective of Magmatic Rocks

    doi: 10.3799/dqkx.2020.160

    • School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

    • Received Date: 2020-05-10
    • Publish Date: 2020-07-15
      Abstract
    • The nature of the Tibetan extremely thick crust and its thickening mechanism are important scientific problems. According to the investigation of igneous rocks,especially Nd and Hf isotope studies,it proved the coexistence of two types of crust (juvenile and reworked) in the Tibetan Plateau,which controls the distribution of different types of ore deposits. The Tibetan crustal thickening was made by both tectonic compression and the input of mantle components carried by magmatism. The timing of the Tibetan crustal thickening was likely in the period of 50-25 Ma.Continental collision zones may be sites of net crustal growth through process of syncollisional magmatism.

       

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