Partial melting of the Appin Quartzite driven by fracture-controlled H[sub]2O infiltration in the aureole of the Ballachulish Igneous Complex, Scottish Highlands

Holness, Marian B. and Clemens, John D. (1999) Partial melting of the Appin Quartzite driven by fracture-controlled H[sub]2O infiltration in the aureole of the Ballachulish Igneous Complex, Scottish Highlands. Contributions to Mineralogy and Petrology, 136(1-2), pp. 154-168. ISSN (print) 0010-7999

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Item Type: Article
Additional Information: This work was supported by the Natural Environment Research Council [grant number GR9/1589].
Uncontrolled Keywords: Scotland, evolution, rock, crystallization, granite, model
Research Area: Earth systems and environmental sciences
Faculty, School or Research Centre: Faculty of Science (until 2011)
Depositing User: Kim Forbes
Date Deposited: 17 Jul 2008
Last Modified: 14 Jun 2011 12:39
URI: http://eprints.kingston.ac.uk/id/eprint/2908

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