Metamorphic reaction rate controlled by fluid pressure not confining pressure: implications of dehydration experiments with gypsum

dc.contributor.author	Llana Fúnez, Sergio
dc.contributor.author	Wheeler, John
dc.contributor.author	Faulkner, Daniel R.
dc.date.accessioned	2013-01-30T10:12:33Z
dc.date.available	2013-01-30T10:12:33Z
dc.date.issued	2012
dc.identifier.citation	Contributions to Mineralogy and Petrology, 164(1), p. 69-79 (2012); doi:10.1007/s00410-012-0726-8	spa
dc.identifier.issn	0010-7999
dc.identifier.uri	http://hdl.handle.net/10651/9273
dc.format.extent	p. 69-79	spa
dc.language.iso	eng
dc.relation.ispartof	Contributions to Mineralogy and Petrology	spa
dc.rights	(c) Contributions to Mineralogy and Petrology
dc.source	SCOPUS	spa
dc.title	Metamorphic reaction rate controlled by fluid pressure not confining pressure: implications of dehydration experiments with gypsum	spa
dc.type	journal article
dc.identifier.local	20120295	spa
dc.identifier.doi	10.1007/s00410-012-0726-8
dc.relation.publisherversion	http://dx.doi.org/10.1007/s00410-012-0726-8	spa

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