Thermobarometric implications of temporal and spatial variability in hydrothermal fluid SiO2-Cl abundances through a full eruptive cycle at 9°50'N East Pacific Rise

Details Thermobarometric implications of temporal and spatial variability in hydrothermal fluid SiO2-Cl abundances through a full eruptive cycle at 9°50'N East Pacific Rise Thermobarometric implications of temporal and spatial variability in hydrothermal fluid SiO2-Cl abundances through a full eruptive cycle at 9°50'N East Pacific Rise

Jun 2009

adsabs.harvard.edu/abs/2009gecas..73q1395v

Geochimica et Cosmochimica Acta Supplement, Volume 73, p.A1395

Physics

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