Mineral carbonation of peridotite fueled by magmatic degassing and melt impregnation in an oceanic transform fault. [PDF]
Klein F +8 more
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Incipient carbonate melting drives metal and sulfur mobilization in the mantle. [PDF]
Ezad IS +6 more
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Inefficient melt mixing below a fast-spreading ridge revealed by Hess Deep lower gabbros (ODP Leg 147 and IODP Expedition 345). [PDF]
Basch V +5 more
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The constant oxidation state of Earth's mantle since the Hadean. [PDF]
Zhang F +6 more
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Depth of slab breakoff in Archean: the role of radiogenic heat production of continental crust and eclogitization of oceanic crust. [PDF]
Fan YL, Zhang LF, Wang Y, Li ZH.
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Formation of Natural Magnesium Silica Hydrate (M-S-H) and Magnesium Alumina Silica Hydrate (M-A-S-H) Cement. [PDF]
Austrheim H +3 more
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Decoupling of high-pressure H2 production from serpentinization and magnetite in subduction zones
Siron G +4 more
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Weathering crusts on peridotite
Contributions to Mineralogy and Petrology, 2015Chemical weathering of dark-green massive peridotite, including partly serpentinized peridotite, produces a distinct and remarkable brown weathering rind when exposed to the atmosphere long enough. The structure and mineral composition of crusts on rocks from the Ronda peridotite, Spain, have been studied in some detail.
Bucher, Kurt +2 more
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