Abstract
ABSTRACT Oxidation and hydration of DSDP Leg 37 basalts occur within, and immediately adjacent to channelways such as cracks, vesicles, and breccias and are a consequence of the movement of fluids, most likely seawater, through such permeable areas. There is no evidence to ...
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CITATION STYLE
Andrews, A. J., Barnett, R. L., MacClement, B. A. E., Fyfe, W. S., Morrison, G., MacRae, N. D., & Starkey, J. (1977). Zeolite Facies Metamorphism, Geochemistry and Some Aspects of Trace Element Redistribution in Altered Basalts of DSDP, Leg 37. In Initial Reports of the Deep Sea Drilling Project, 37. U.S. Government Printing Office. https://doi.org/10.2973/dsdp.proc.37.162.1977
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