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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

Citation

Kamenetsky, VS and Kamenetsky, MB, Magmatic fluids immiscible with silicate melts: examples from inclusions in phenocrysts and glasses, and implications for magma evolution and metal transport, Frontiers in Geofluids, Wiley-Blackwell, B Yardley, C Manning, G Garven (ed), Chichester UK, pp. 293-311. ISBN 978-1-4443-3330-5 (2011) [Research Book Chapter]


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Copyright Statement

Copyright 2011 Wiley-Blackwell.

Official URL: http://au.wiley.com/WileyCDA/WileyTitle/productCd-...

DOI: doi:10.1002/9781444394900.ch20

Abstract

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

Item Details

Item Type:Research Book Chapter
Keywords:immiscibility melt inclusions mgmatic process
Research Division:Earth Sciences
Research Group:Geology
Research Field:Igneous and Metamorphic Petrology
Objective Division:Expanding Knowledge
Objective Group:Expanding Knowledge
Objective Field:Expanding Knowledge in the Earth Sciences
Author:Kamenetsky, VS (Professor Vadim Kamenetsky)
Author:Kamenetsky, MB (Dr Maya Kamenetsky)
ID Code:74905
Year Published:2011
Deposited By:Centre for Ore Deposit Research - CODES CoE
Deposited On:2011-12-15
Last Modified:2018-04-05
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