A role for subducted super-hydrated kaolinite in Earth’s deep water cycle
A role for subducted super-hydrated kaolinite in Earth’s deep water cycle
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Author / Creator
Hwang, Huijeong , Seoung, Donghoon , Lee, Yongjae , Liu, Zhenxian , Liermann, Hanns-Peter , Cynn, Hyunchae , Vogt, Thomas , Kao, Chi-Chang , Mao, Ho-Kwang , Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States) and SLAC National Accelerator Laboratory (SLAC), Menlo Park, CA (United States)
Publisher
United States: Nature Publishing Group
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English
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United States: Nature Publishing Group
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Contents
Water is the most abundant volatile component in the Earth. It continuously enters the mantle through subduction zones, where it reduces the melting temperature of rocks to generate magmas. The dehydration process in subduction zones, which determines whether water is released from the slab or transported into the deeper mantle, is an essential com...
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Full title
A role for subducted super-hydrated kaolinite in Earth’s deep water cycle
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TN_cdi_osti_scitechconnect_1423465
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_osti_scitechconnect_1423465
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ISSN
1752-0894
E-ISSN
1752-0908
