Fluid-rock interactions in the lower oceanic crust: Thermodynamic models of hydrothermal alteration

Rocks from the lower oceanic crust show both petrologic and isotopic evidence for extensive alteration by circulating hydrothermal fluids derived from seawater. Deeply circulating fluids may have a substantial, but as yet largely undetermined, impact on the thermal regime of spreading centers, magma...

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Veröffentlicht in:	Journal of Geophysical Research. B 1998-01, Vol.103 (B1), p.547-575
Hauptverfasser:	McCollom, Thomas M., Shock, Everett L.
Format:	Artikel
Sprache:	eng
Schlagworte:	Crystalline rocks Earth sciences Earth, ocean, space Exact sciences and technology Igneous and metamorphic rocks petrology, volcanic processes, magmas Marine
Online-Zugang:	Volltext
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