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Roffeis, C., Corfu, F., Austrheim, H. (2012) Evidence for a Caledonian amphibolite to eclogite facies pressure gradient in the Middle Allochthon Lindås Nappe, SW-Norway. Contributions to Mineralogy and Petrology, 164 (1) 81-99 doi:10.1007/s00410-012-0727-7

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Reference TypeJournal (article/letter/editorial)
TitleEvidence for a Caledonian amphibolite to eclogite facies pressure gradient in the Middle Allochthon Lindås Nappe, SW-Norway
JournalContributions to Mineralogy and Petrology
AuthorsRoffeis, C.Author
Corfu, F.Author
Austrheim, H.Author
Year2012 (July)Volume164
Issue1
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s00410-012-0727-7Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID79342Long-form Identifiermindat:1:5:79342:3
GUID0
Full ReferenceRoffeis, C., Corfu, F., Austrheim, H. (2012) Evidence for a Caledonian amphibolite to eclogite facies pressure gradient in the Middle Allochthon Lindås Nappe, SW-Norway. Contributions to Mineralogy and Petrology, 164 (1) 81-99 doi:10.1007/s00410-012-0727-7
Plain TextRoffeis, C., Corfu, F., Austrheim, H. (2012) Evidence for a Caledonian amphibolite to eclogite facies pressure gradient in the Middle Allochthon Lindås Nappe, SW-Norway. Contributions to Mineralogy and Petrology, 164 (1) 81-99 doi:10.1007/s00410-012-0727-7
In(2012, July) Contributions to Mineralogy and Petrology Vol. 164 (1) Springer Science and Business Media LLC

See Also

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Glodny, Johannes, Kühn, Alexander, Austrheim, Håkon (2008) Geochronology of fluid-induced eclogite and amphibolite facies metamorphic reactions in a subduction–collision system, Bergen Arcs, Norway. Contributions to Mineralogy and Petrology, 156 (1) 27-48 doi:10.1007/s00410-007-0272-y
Lundmark, A. M., Corfu, F. (2008) Late-orogenic Sveconorwegian massif anorthosite in the Jotun Nappe Complex, SW Norway, and causes of repeated AMCG magmatism along the Baltoscandian margin. Contributions to Mineralogy and Petrology, 155 (2) 147-163 doi:10.1007/s00410-007-0233-5
Corfu, F., Ravna, E. J. K., Kullerud, K. (2003) A Late Ordovician U?Pb age for the Troms? Nappe eclogites, Uppermost Allochthon of the Scandinavian Caledonides. Contributions to Mineralogy and Petrology, 145 (4) 502-513 doi:10.1007/s00410-003-0466-x
Heinrich, Christoph A. (1982) Kyanite-eclogite to amphibolite fades evolution of hydrous mafic and pelitic rocks, Adula nappe, Central Alps. Contributions to Mineralogy and Petrology, 81 (1) 30-38 doi:10.1007/bf00371156
(2019) The granulite- to eclogite- and amphibolite-facies transition: a volume and mass transfer study in the Lindås Nappe, Bergen Arcs, west Norway. Special Publication, 478. Geological Society of London. 241-264 doi:10.1144/sp478.9
Bingen, Bernard, Austrheim, Håkon, Whitehouse, Martin J., Davis, William J. (2004) Trace element signature and U–Pb geochronology of eclogite-facies zircon, Bergen Arcs, Caledonides of W Norway. Contributions to Mineralogy and Petrology, 147 (6) 671-683 doi:10.1007/s00410-004-0585-z
Root, David, Corfu, Fernando (2012) U–Pb geochronology of two discrete Ordovician high-pressure metamorphic events in the Seve Nappe Complex, Scandinavian Caledonides. Contributions to Mineralogy and Petrology, 163 (5) 769-788 doi:10.1007/s00410-011-0698-0
Jakobsson, Sigurdur (2012) Oxygen fugacity control in piston-cylinder experiments. Contributions to Mineralogy and Petrology, 164 (3) 397-406 doi:10.1007/s00410-012-0743-7
Bingen, B. (1998) Zircon Growth During Fluid Induced Caledonian/Scandian Eclogite-facies Metamorphism of the Lindås Nappe, Caledonides of W Norway. Mineralogical Magazine, 62 (1) 161-162 doi:10.1180/minmag.1998.62a.1.86
Green, David H., Rosenthal, Anja, Kovács, István (2012) Comment on “The beginnings of hydrous mantle wedge melting”, CB Till, TL Grove, AC Withers, Contributions to Mineralogy and Petrology, DOI 10.1007/s00410-011-0692-6. Contributions to Mineralogy and Petrology, 164 (6) 1077-1081 doi:10.1007/s00410-012-0802-0
Owens, Brent E., Dymek, Robert F. (1997) Comparative petrology of Archaean anorthosites in amphibolite and granulite facies terranes, SW Greenland. Contributions to Mineralogy and Petrology, 128 (4) 371-384 doi:10.1007/s004100050315
 
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