Volume 47 Issue 7
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Hu Hang, Yu Xing, Han Xiqiu, 2022. Quantitative Constraints of Subduction Cycle Components on Oceanic Mantle Heterogeneity. Earth Science, 47(7): 2616-2630. doi: 10.3799/dqkx.2021.057
Citation: Hu Hang, Yu Xing, Han Xiqiu, 2022. Quantitative Constraints of Subduction Cycle Components on Oceanic Mantle Heterogeneity. Earth Science, 47(7): 2616-2630. doi: 10.3799/dqkx.2021.057
shu

Quantitative Constraints of Subduction Cycle Components on Oceanic Mantle Heterogeneity

doi: 10.3799/dqkx.2021.057
  • 1.

    Key Laboratory of Submarine Geosciences & Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China

  • 2.

    School of Oceanography, Shanghai Jiao Tong University, Shanghai 200240, China

  • Received Date: 2021-03-10
  • Publish Date: 2022-07-25
    Abstract
  • There is a wide range of heterogeneity in the oceanic mantle, which can be caused by a variety of models, among which the subduction cycle has an important influence on the composition of the mantle. In order to clarify the relative contribution of each cyclic component to the reformation of depleted mantle and the enrichment source region, in this paper it systematically summarizes the average trace element characteristics of different cyclic components (pelagic sediments, subducted oceanic crust, continental crust), and the cyclic components undergone chemical changes during subduction are calculated. Based on the modified cyclic components, the mixing and melting simulations with depleted mantle sources are carried out. It is found that the HIMU basalt can be formed by a low degree of melting (0.5%-1.5%) in the mantle formed by the mixing of pure subducted oceanic crust (≤10%) and depleted mantle (≥90%). The EMI basalts can be formed by a low degree of melting (1%-2%) in the mantle formed by the mixing of subducted oceanic crust (≤10%), low continental crust (≤3%) and depleted mantle (≥90%). The EMII basalts can be formed by a low degree of melting (1%-1.5%) in the mantle formed by the mixing of subducted oceanic crust (≤10%), GLOSS-II(global subducting sediment) or upper continental crust (≤0.8%) and depleted mantle (≥90%).

     

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