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(2014) Pressure–temperature evolution of a kyanite–garnet pelitic gneiss from Åreskutan: evidence of ultra-high-pressure metamorphism of the Seve Nappe Complex, west-central Jämtland, Swedish Caledonides. Special Publication, 390. Geological Society of London. 321-336 doi:10.1144/sp390.7

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TitlePressure–temperature evolution of a kyanite–garnet pelitic gneiss from Åreskutan: evidence of ultra-high-pressure metamorphism of the Seve Nappe Complex, west-central Jämtland, Swedish Caledonides
ReportSpecial Publication
Year2014Volume390
PublisherGeological Society of London
DOIdoi:10.1144/sp390.7Search in ResearchGate
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Mindat Ref. ID439393Long-form Identifiermindat:1:5:439393:5
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Full Reference(2014) Pressure–temperature evolution of a kyanite–garnet pelitic gneiss from Åreskutan: evidence of ultra-high-pressure metamorphism of the Seve Nappe Complex, west-central Jämtland, Swedish Caledonides. Special Publication, 390. Geological Society of London. 321-336 doi:10.1144/sp390.7
Plain Text(2014) Pressure–temperature evolution of a kyanite–garnet pelitic gneiss from Åreskutan: evidence of ultra-high-pressure metamorphism of the Seve Nappe Complex, west-central Jämtland, Swedish Caledonides. Special Publication, 390. Geological Society of London. 321-336 doi:10.1144/sp390.7
In(2014) Special Publication Vol. 390. Geological Society of London

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(2014) Pressure–temperature estimates on the Tjeliken eclogite: new insights into the (ultra)-high-pressure evolution of the Seve Nappe Complex in the Scandinavian Caledonides. Special Publication, 390. Geological Society of London. 369-384 doi:10.1144/sp390.14
Majka, J., Janák, M., Andersson, B., Klonowska, I., Gee, D. G., Rosén, Å., & Kośmińska, K. (2014). Pressure–temperature estimates on the Tjeliken eclogite: new insights into the (ultra)-high-pressure evolution of the Seve Nappe Complex in the Scandinavian Caledonides. Geological Society, London, Special Publications, 390(1), 369-384.
(1989) Pressure, temperature and structural evolution of the Sulitjelma fold-nappe, central Scandinavian Caledonides. Special Publication, 43. Geological Society of London. 391-411 doi:10.1144/gsl.sp.1989.043.01.36
Majka, J., Janák, M., Andersson, B., Klonowska, I., Gee, D.G., Rosén, Å., & Kośminska, K. (2014): Pressure-temperature estimates on the Tjeliken eclogite: new insights into the (ultra)-high pressure evolution of the Seve Nappe Complex in the Scandinavian Caledonides; in: F. Corfu, D. Gasser & D.M. Chew (Eds.) New Perspectives on the Caledonides of Scandinavia and Related Areas (pp. 369–384). Geological Society, London, Special Publications: 390. DOI: 10.1144/SP390.14
Zagórska, A. (2020) U-Pb Zircon Dating of Migmatitic Paragneisses and Garnet Amphibolite from the High Pressure Seve Nappe Complex in Kittalfjäll, Swedish Caledonides. Minerals 10, 295.
(2014) Tectonometamorphic evolution of the Åreskutan Nappe – Caledonian history revealed by SIMS U–Pb zircon geochronology. Special Publication, 390. Geological Society of London. 337-368 doi:10.1144/sp390.10
(2014) Tectonic reconstruction and sediment provenance of a far-travelled oceanic nappe, Helgeland Nappe Complex, west-central Norway. Special Publication, 390. Geological Society of London. 583-602 doi:10.1144/sp390.3
(2014) Metamorphic constraints on the Caledonian Upper Allochthon of Central Norway: the Gula Complex staurolite–garnet–kyanite mica schist. Special Publication, 390. Geological Society of London. 563-581 doi:10.1144/sp390.6
Janák, Marian, van Roermund, Herman, Majka, Jarosław, Gee, David (2013) UHP metamorphism recorded by kyanite-bearing eclogite in the Seve Nappe Complex of northern Jämtland, Swedish Caledonides. Gondwana Research, 23 (3) 865-879 doi:10.1016/j.gr.2012.06.012
(2014) Evolution and origin of the Revsegg Nappe in the SW-Norwegian Caledonides: an allochthon with Ordovician elements. Special Publication, 390. Geological Society of London. 525-539 doi:10.1144/sp390.8
(2014) The Bratten–Landegode gneiss complex: a fragment of Laurentian continental crust in the Uppermost Allochthon of the Scandinavian Caledonides. Special Publication, 390. Geological Society of London. 633-654 doi:10.1144/sp390.1
 
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