Volume 44 Issue 12
Dec.  2019
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Li Dongyong, Xiao Yilin, Wang Yangyang, Shen Ji, Liu Haiyang, 2019. Mg-Li-Fe-Cr Isotopic Fractionation during Subduction. Earth Science, 44(12): 4081-4085. doi: 10.3799/dqkx.2019.255
Citation: Li Dongyong, Xiao Yilin, Wang Yangyang, Shen Ji, Liu Haiyang, 2019. Mg-Li-Fe-Cr Isotopic Fractionation during Subduction. Earth Science, 44(12): 4081-4085. doi: 10.3799/dqkx.2019.255

Mg-Li-Fe-Cr Isotopic Fractionation during Subduction

doi: 10.3799/dqkx.2019.255
  • Received Date: 2019-08-30
  • Publish Date: 2019-12-15
  • In order to investigate mantle heterogeneities induced by subducted crustal plate, many studies have been focused on geochemical characteristics of stable metal isotopic systematics in subduction zone in recent years. Limited Mg isotopic fractionation occurred during subduction and exhumation, thus lighter Mg isotopic composition of continental basalts might be caused by carbonatite metasomatism. Instead of inherited Li isotopes of amphibolite, eclogite has lighter Li isotopies, which are attributed to kinetic diffusion, dehydration, or rehydration. Isotopes of Fe and Cr have insignificant fractionation during formation of eclogite, however, Fe and Cr isotopic composition of serpentinite are related to oxidation index, suggesting dehydration or alteration of fluids during serpentinization could shift Fe and Cr isotopic composition of serpentinite.

     

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