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Holness, Marian B., Clemens, John D. (1999) Partial melting of the Appin Quartzite driven by fracture-controlled H 2 O infiltration in the aureole of the Ballachulish Igneous Complex, Scottish Highlands. Contributions to Mineralogy and Petrology, 136 (1) 154-168 doi:10.1007/s004100050529

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Reference TypeJournal (article/letter/editorial)
TitlePartial melting of the Appin Quartzite driven by fracture-controlled H 2 O infiltration in the aureole of the Ballachulish Igneous Complex, Scottish Highlands
JournalContributions to Mineralogy and Petrology
AuthorsHolness, Marian B.Author
Clemens, John D.Author
Year1999 (July 15)Volume136
Issue1
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s004100050529Search in ResearchGate
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Mindat Ref. ID77792Long-form Identifiermindat:1:5:77792:0
GUID0
Full ReferenceHolness, Marian B., Clemens, John D. (1999) Partial melting of the Appin Quartzite driven by fracture-controlled H 2 O infiltration in the aureole of the Ballachulish Igneous Complex, Scottish Highlands. Contributions to Mineralogy and Petrology, 136 (1) 154-168 doi:10.1007/s004100050529
Plain TextHolness, Marian B., Clemens, John D. (1999) Partial melting of the Appin Quartzite driven by fracture-controlled H 2 O infiltration in the aureole of the Ballachulish Igneous Complex, Scottish Highlands. Contributions to Mineralogy and Petrology, 136 (1) 154-168 doi:10.1007/s004100050529
In(1999, July) Contributions to Mineralogy and Petrology Vol. 136 (1) Springer Science and Business Media LLC

See Also

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Holness, M. B. (1998) Contrasting rock permeability in the aureole of the Ballachulish igneous complex, Scottish Highlands: the influence of surface energy?. Contributions to Mineralogy and Petrology, 131 (1) 86-94 doi:10.1007/s004100050380
Clemens, John D., Holness, Marian B. (2000) Textural evolution and partial melting of arkose in a contact aureole: a case study and implications. Visual Geosciences, 5 (4). 1-14 doi:10.1007/s10069-000-0004-1
Holness, Marian B. (2014) The effect of crystallization time on plagioclase grain shape in dolerites. Contributions to Mineralogy and Petrology, 168 (5) doi:10.1007/s00410-014-1076-5
Naslund, H. R. (1986) Disequilibrium partial melting and rheomorphic layer formation in the contact aureole of the Basistoppen sill, East Greenland. Contributions to Mineralogy and Petrology, 93 (3) 359-367 doi:10.1007/bf00389394
McMillan, Andy, Harris, Nigel B. W., Holness, Marian, Ashwal, Lewis, Kelley, Simon, Rambeloson, Roger (2003) A granite?gabbro complex from Madagascar: constraints on melting of the lower crust. Contributions to Mineralogy and Petrology, 145 (5) 585-599 doi:10.1007/s00410-003-0470-1
Kaufmann, Felix E. D., Vukmanovic, Zoja, Holness, Marian B., Hecht, Lutz (2018) Orthopyroxene oikocrysts in the MG1 chromitite layer of the Bushveld Complex: implications for cumulate formation and recrystallisation. Contributions to Mineralogy and Petrology, 173 (2) doi:10.1007/s00410-018-1441-x
Ferry, John M. (1996) Prograde and retrograde fluid flow during contact metamorphism of siliceous carbonate rocks from the Ballachulish aureole, Scotland. Contributions to Mineralogy and Petrology, 124 (3) 235-254 doi:10.1007/s004100050189
Fraser, G.L., Pattison, D.R.M., Heaman, L.M. (2004) Age of the Ballachulish and Glencoe Igneous Complexes (Scottish Highlands), and paragenesis of zircon, monazite and baddeleyite in the Ballachulish Aureole. Journal of the Geological Society, 161 (3) 447-462 doi:10.1144/0016-764903-018
Pattison, David R. M., Harte, Ben (1997) The geology and evolution of the Ballachulish Igneous Complex and Aureole. Scottish Journal of Geology, 33 (1) 1-29 doi:10.1144/sjg33010001
Rudge, John F., Holness, Marian B., Smith, Graham C. (2008) Quantitative textural analysis of packings of elongate crystals. Contributions to Mineralogy and Petrology, 156 (4) 413-429 doi:10.1007/s00410-008-0293-1
Holness, Marian B., Farr, Robert, Neufeld, Jerome A. (2017) Crystal settling and convection in the Shiant Isles Main Sill. Contributions to Mineralogy and Petrology, 172 (1) doi:10.1007/s00410-016-1325-x
 
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