Garnet secondary ion mass spectrometry oxygen isotopes reveal crucial roles of pulsed magmatic fluid and its mixing with meteoric water in lode gold genesis
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DOI: 10.1073/pnas.2116380119
Abstract: Significance There is a common consensus that lode gold deposits mostly precipitated from metamorphic fluids via fluid boiling and/or fluid–rock interaction, but whether magmatic hydrothermal fluids and the mixing of such fluids with an external… read more here.
Keywords: secondary ion; garnet secondary; lode gold; lode ... See more keywords