Hydrogen and oxygen isotopic compositions of serpentinite and their influencing factors
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Publisher
China Science Publishing & Media Ltd.
Link
https://engine.scichina.com/doi/pdf/21FFCB3ADBDD4E61B7996107D7590695
Reference57 articles.
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2. Agrinier P, Hékinian R, Bideau D, Javoy M. 1995. O and H stable isotope compositions of oceanic crust and upper mantle rocks exposed in the Hess Deep near the Galapagos Triple Junction. Earth and Planetary Science Letters, 136(3–4): 183–196.
3. Albers E, Kahl W A, Beyer L, Bach W. 2020. Variant across-forearc compositions of slab-fluids recorded by serpentinites: Implications on the mobilization of FMEs from an active subduction zone (Mariana forearc). Lithos, 364–365: 105525.
4. Alt J C, Garrido C J, Shanks W C, Turchyn A, Padr\′on-Navarta J A, Sánchez-Vizcaíno V L, Pugnaire M T G, Marchesi C. 2012. Recycling of water, carbon, and sulfur during subduction of serpentinites: A stable isotope study of Cerro del Almirez, Spain. Earth and Planetary Science Letters, 327: 50–60.
5. Alt J, Shanksiii W. 2006. Stable isotope compositions of serpentinite seamounts in the Mariana forearc: Serpentinization processes, fluid sources and sulfur metasomatism. Earth and Planetary Science Letters, 242(3–4): 272–285.
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