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Williams, I. S., Claesson, S. (1987) Isotopic evidence for the Precambrian provenance and Caledonian metamorphism of high grade paragneisses from the Seve Nappes, Scandinavian Caledonides. Contributions to Mineralogy and Petrology, 97 (2) 205-217 doi:10.1007/bf00371240

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Reference TypeJournal (article/letter/editorial)
TitleIsotopic evidence for the Precambrian provenance and Caledonian metamorphism of high grade paragneisses from the Seve Nappes, Scandinavian Caledonides
JournalContributions to Mineralogy and Petrology
AuthorsWilliams, I. S.Author
Claesson, S.Author
Year1987 (October)Volume97
Issue2
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/bf00371240Search in ResearchGate
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Mindat Ref. ID76105Long-form Identifiermindat:1:5:76105:3
GUID0
Full ReferenceWilliams, I. S., Claesson, S. (1987) Isotopic evidence for the Precambrian provenance and Caledonian metamorphism of high grade paragneisses from the Seve Nappes, Scandinavian Caledonides. Contributions to Mineralogy and Petrology, 97 (2) 205-217 doi:10.1007/bf00371240
Plain TextWilliams, I. S., Claesson, S. (1987) Isotopic evidence for the Precambrian provenance and Caledonian metamorphism of high grade paragneisses from the Seve Nappes, Scandinavian Caledonides. Contributions to Mineralogy and Petrology, 97 (2) 205-217 doi:10.1007/bf00371240
In(1987, October) Contributions to Mineralogy and Petrology Vol. 97 (2) Springer Science and Business Media LLC

See Also

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Claesson, Stefan (1987) Isotopic evidence for the Precambrian provenance and Caledonian metamorphism of high grade paragneisses from the Seve Nappes, Scandinavian Caledonides. Contributions to Mineralogy and Petrology, 97 (2) 196-204 doi:10.1007/bf00371239
Kullerud, K., Stephens, M. B., Zachrisson, E. (1990) Pillow lavas as protoliths for eclogites: evidence from a late Precambrian-Cambrian continental margin, Seve Nappes, Scandinavian Caledonides. Contributions to Mineralogy and Petrology, 105 (1) 1-10 doi:10.1007/bf00320962
Claesson, Stefan (1986) U—Pb ion microprobe studies of high-grade paragneisses from the Seve Nappes, Swedish Caledonides. Geologiska Föreningen i Stockholm Förhandlingar, 108 (3) 276 doi:10.1080/11035898609454703
Gromet, L.P., Sjöström, H., Bergman, S., Claesson, S., Essex, R.M., AndrĂ©asson, P.G., Albrecht, L. (1996) Contrasting ages of metamorphism in the Seve nappes: U‐Pb results from the central and northern Swedish Caledonides. GFF, 118. 36-37 doi:10.1080/11035899609546308
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
Claesson, Stefan (1982) Caledonian metamorphism of Proterozoic Seve rocks on Mt. Åreskutan, southern Swedish Caledonides. Geologiska Föreningen i Stockholm Förhandlingar, 103 (3) 291-304 doi:10.1080/11035898209453700
van Roermund, Herman L. M., Bakker, Ebo (1983) Structure and metamorphism of the TĂ„ngen—Inviken area, Seve Nappes, Central Scandinavian Caledonides. Geologiska Föreningen i Stockholm Förhandlingar, 105 (4) 301-319 doi:10.1080/11035898309454568
Patchett, P. Jonathan, Ruiz, Joaquin (1987) Nd isotopic ages of crust formation and metamorphism in the Precambrian of eastern and southern Mexico. Contributions to Mineralogy and Petrology, 96 (4) 523-528 doi:10.1007/bf01166697
Crowley, Peter D., Spear, Frank S. (1987) The P-T evolution of the Middle Köli Nappe Complex, Scandinavian Caledonides (68° N) and its tectonic implications. Contributions to Mineralogy and Petrology, 95 (4) 512-522 doi:10.1007/bf00402209
Gruau, G., Tourpin, S., Fourcade, S., Blais, S. (1992) Loss of isotopic (Nd, O) and chemical (REE) memory during metamorphism of komatiites: new evidence from eastern Finland. Contributions to Mineralogy and Petrology, 112 (1) 66-82 doi:10.1007/bf00310956
MĂžrk, Mai Britt E., Kullerud, KĂ„re, Stabel, Arne (1988) Sm-Nd dating of Seve eclogites, Norrbotten, Sweden - Evidence for early Caledonian (505 Ma) subduction. Contributions to Mineralogy and Petrology, 99 (3) 344-351 doi:10.1007/bf00375366
 
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