Volume 44 Issue 12
Dec.  2019
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Zheng Yongfei, Chen Yixiang, 2019. Crust-Mantle Interaction in Continental Subduction Zones. Earth Science, 44(12): 3961-3983. doi: 10.3799/dqkx.2019.982
Citation: Zheng Yongfei, Chen Yixiang, 2019. Crust-Mantle Interaction in Continental Subduction Zones. Earth Science, 44(12): 3961-3983. doi: 10.3799/dqkx.2019.982
shu

Crust-Mantle Interaction in Continental Subduction Zones

doi: 10.3799/dqkx.2019.982
  • 1.

    CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China

  • 2.

    Center of Excellence for Comparative Planetology, Chinese Academy of Sciences, Hefei 230026, China

  • Received Date: 2019-10-08
  • Publish Date: 2019-12-15
    Abstract
  • The recycling of crustal material into the mantle by subduction is the first-order mechanism of Earth's interior. In order to decipher the crustal-mantle interaction in subduction zones,it is important to distinguish different types of metasomatism by subducting crust-derived fluids such as aqueous solutions and hydrous melts to the mantle wedge. For this purpose,various lines of petrological and geochemical evidence have been used to determine the physicochemical properties of subduction zone fluids at the slab-mantle interface in subduction channels. In doing so,it is critical to determine how crustal rocks underwent metamorphic dehydration and partial melting at mantle depths. After incorporation of subduction zone fluids into the mantle wedge,different compositions of mantle metasomatites were generated in the mantle wedge to result in mantle heterogeneities. As soon as these metasomatites underwent partial melting,mafic igneous rocks were produced with both petrological and geochemical signatures of the subducted crust and the mantle wedge. In this regard,such processes as metamorphism,metasomatism and magmatism in subduction zones are the keys to the recycling of crustal material at convergent plate boundaries. The mantle wedge is the key lithotectonic unit linking the subducting slab and the obducting plate and thus plays an important role in the material transport and energy exchange in the subduction system. The orogenic mantle wedge peridotite directly records different types of crustal metasomatism in subduction zones. Subduction zone magmatism is the manifestation for recycling of subducted oceanic and continental rocks. These rocks witness the processes of magmatic melts from the mantle wedge to crustal levels above subduction zones,providing the natural samples to decode indirectly the crustal recycling at convergent plate boundaries. Although there are many advances in the study of subduction zones with respect to the crust-mantle interaction,such three processes as metamorphism,metasomatism and magmatism in subduction zones are still the most important targets in the deep Earth science. Many key problems cannot be resolved if no sufficient attention is paid to an integrated study of these three aspects. Such problems include the physiochemical properties of subduction zone fluids,the mechanism and process of crust-mantle interaction,the material source and triggering mechanism of mantle-derived magmatism above subduction zones,and the impact of deep mantle process on the shallow crustal environments. The future research needs to focus on the key question of material recycling in subduction zones,and take the metamorphism,metasomatism and magmatism in subduction zones as a whole in the framework of Earth system science. This concerns the transport process and the resource and environmental effects of volatile components,and clarify the coupling mechanism of plate subduction and material recycling in deep Earth by intensive studies of paleo-subduction zones.

     

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