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H2 Production from Ultramafic-Bearing Gabbroic Rock Assemblages: An Experimental Study at 420°C, 500 bars
H2 Production from Ultramafic-Bearing Gabbroic Rock Assemblages: An Experimental Study at 420°C, 500 bars
2009
M. E. Rough
William E. Seyfried
Keywords:
Petrology
Hydrothermal vent
Trace element
Bearing (mechanical)
Geophysics
Mid-ocean ridge
Magma chamber
Ultramafic rock
Geology
Hydrothermal circulation
Correction
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