Fluid bubbles in melt inclusions and pillow-rim glasses: high-temperature precursors to hydrothermal fluid?

Hypotheses for the formation of many types of hydrothermal ore deposits often involve the direct contribution of magma-related fluids (e.g., Cu–Mo–Au porphyries) or their superimposition on barren hydrothermal cells (e.g., volcanic-hosted massive sulfide deposits). However, the chemical and phase co...

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Bibliographic Details
Published in:Chemical Geology
Main Authors: Kamenetsky, V.S., Davidson, P., Mernagh, T.P., Crawford, A.J., Gemmell, J.B., Portnyagin, Maxim, Shinjo, R.
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2002
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/1012/
https://oceanrep.geomar.de/id/eprint/1012/1/1-s2.0-S0009254101003837-main.pdf
https://doi.org/10.1016/S0009-2541(01)00383-7