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Under conditions of elevated temperature and pressure, fracture closure and re-mineralization due to serpentinization reactions lead to rapid permeability loss in mafic and ultramafic rocks.
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This page is a summary of: Evolution of fracture permeability of ultramafic rocks undergoing serpentinization at hydrothermal conditions: An experimental study, Geochemistry Geophysics Geosystems, January 2016, American Geophysical Union (AGU),
DOI: 10.1002/2015gc005973.
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