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

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, VS, Davidson, P, Mernagh, TP, Crawford, AJ, Gemmell, JB, Portnyagin, MV, Shinjo, R
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2002
Subjects:
Online Access:https://doi.org/10.1016/S0009-2541(01)00383-7
http://ecite.utas.edu.au/24736