Volume 44 Issue 4
Apr.  2019
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Tang Zengcai, Zhou Hanwen, Hu Kaiming, Chen Zhongda, Wu Xiaoyong, Hu Wenjie, Dong Xuefa, Zhao Xudong, Yu Shengqiang, Zhang Jianfang, 2019. Petrogenesis of Late Mesozoic Granites in Northwest Zhejiang. Earth Science, 44(4): 1278-1294. doi: 10.3799/dqkx.2018.208
Citation: Tang Zengcai, Zhou Hanwen, Hu Kaiming, Chen Zhongda, Wu Xiaoyong, Hu Wenjie, Dong Xuefa, Zhao Xudong, Yu Shengqiang, Zhang Jianfang, 2019. Petrogenesis of Late Mesozoic Granites in Northwest Zhejiang. Earth Science, 44(4): 1278-1294. doi: 10.3799/dqkx.2018.208
shu

Petrogenesis of Late Mesozoic Granites in Northwest Zhejiang

doi: 10.3799/dqkx.2018.208
  • 1.

    Zhejiang Institute of Geological Survey, Hangzhou 311203, China

  • 2.

    School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

  • Received Date: 2018-04-12
  • Publish Date: 2019-04-15
    Abstract
  • The strong Late Mesozoic magmatic intruding events happened in Northwest Zhejiang area, which is located in the active western Pacific margin. The granites are classified as Ⅰ- and aluminous A-types, and the former is further divided into Ⅰ-type and highly fractionated Ⅰ-type granites. The Ⅰ-type granites of Mid-Late Jurassic to early Early Cretaceous(172-135 Ma) have the initial 87Sr/86Sr ratios ranging from 0.707 004 to 0.711 896, εNd(t) values from -6.70 to -2.00, εHf(t) values from -5.08 to -1.67, indicating that these granites are originated from mixing between remelted Meso-Neoproterozoic Jiangnan island arc and little mantle materials rose along slab crack. The formation of these granites may be closely related to the subduction of Paleo-Pacific plate. The highly fractionated Ⅰ-type granites in the early Early Cretaceous(147-135 Ma) have the initial 87Sr/86Sr ratio ranging from 0.706 890 to 0.709 880, εNd(t) values from -6.80 to -4.50, εHf(t) values from -6.59 to -5.23, suggesting that they are the products of magma mixing by remelting crustal materials of the Meso-Neoproterozoic and rising mantle mafic magma due to asthenosphere uplifting. It also indicates that the tectonic environment transformed from compression to extension in this period.The A-type granites of middle Early Cretaceous(135-123 Ma) have the initial 87Sr/86Sr ratios ranging from 0.703 503 to 0.710 171, εNd(t) values from -8.90 to -0.30, εHf(t) values from -9.70 to 2.48, indicating that the magma during Middle-Early Cretaceous was mainly originated from remelting of the Meso-Neoproterozoic crustal materials, mixed by more and more mantle materials, in an extension setting.

     

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