Fluid inclusion petrology and microthermometry of the Cocos Ridge hydrothermal system, IODP Expedition 344 (CRISP 2), Site U1414.

Geochem Geophys Geosyst · 2016 · PMC4985704 · PMID 27570496

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a clear trendno p-value reported

This is based on the argument that the earliest large FI 1A show a clear trend to decrepitation and their high homogenization temperatures, i.e., low densities, cannot be related to a primary origin.

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