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Magmatic fluids immiscible with silicate melts: examples from inclusions in phenocrysts and glasses, and implications for magma evolution and metal transport
In this paper, several examples of recent research on melt and fluid inclusions are used to demonstrate the significance of naturally occurring immiscibility in understanding some large-scale magma chamber processes such as degassing and partitioning of metals
History
Publication title
Frontiers in GeofluidsEditors
B Yardley, C Manning, G GarvenPagination
293-311ISBN
978-1-4443-3330-5Department/School
School of Natural SciencesPublisher
Wiley-BlackwellPlace of publication
Chichester UKExtent
20Rights statement
Copyright 2011 Wiley-Blackwell.Repository Status
- Restricted