Rate of antigorite dehydration at 2 GPa applied to subduction zones

David H. Eggler; Amy N. Ehmann

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Rate of antigorite dehydration at 2 GPa applied to subduction zones

机译：应用于俯冲带的2 GPa防蛇纹石脱水率

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A mixture of antigorite, forsterite, and enstatite was reacted at 2 GPa pressure, with water, to study kinetics of the reaction Mg₄₈Si₃₄O₈₅(OH)₆₂ = 10 Mg₂Si₂O₆ + 14 Mg₂SiO₄ + 31 H₂O.

机译：在2 GPa的压力下，将水蛇纹石，镁橄榄石和顽辉石的混合物与水进行反应，以研究该反应的动力学。 Mg _{48 Si < sub> 34 O _{85 （OH）_{62 = 10 Mg _{2 Si _{2 O _{6 + 14 Mg _{2 SiO _{4 + 31 H _{2 O.}}}}}}}}}

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《American Mineralogist》 |2010年第6期|761-769|共9页
作者
David H. Eggler; Amy N. Ehmann;
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Department of Geosciences, The Pennsylvania State University, University Park, Pennsylvania 16802, U.S.A.;

Department of Geosciences, The Pennsylvania State University, University Park, Pennsylvania 16802, U.S.A.;

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1. Rate of antigorite dehydration at 2 GPa applied to subduction zones [J] . DaviD H. EgglEr, amy n. EHmann The American mineralogist . 2010,第5a6期

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3. Fluid-mediated carbon release from serpentinite-hosted carbonates during dehydration of antigorite-serpentinite in subduction zones [J] . Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System . 2020,第期

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7. The intrinsic nature of antigorite breakdown at 3 GPa: Experimental constraints on redox conditions of serpentinite dehydration in subduction zones [O] . Juliette Maurice, Nathalie Bolfan-Casanova, Sylvie Demouchy, 2020

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Rate of antigorite dehydration at 2 GPa applied to subduction zones

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