Isotopic evidence for the Precambrian provenance and Caledonian metamorphism of high grade paragneisses from the Seve Nappes, Scandinavian Caledonides-Reference-Cited by-同舟云学术

Isotopic evidence for the Precambrian provenance and Caledonian metamorphism of high grade paragneisses from the Seve Nappes, Scandinavian Caledonides

Published:1987-10 Issue:2 Volume:97 Page:196-204
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contr. Mineral. and Petrol.

Author:

Claesson Stefan

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF00371239.pdf

Reference43 articles.

1. Allégre CJ, Othman DB (1980) Nd-Sr isotopic relationship in granitoid rocks and continental crust development:a chemical approach to orogenesis. Nature 286:335?342

2. Armstrong RL (1981) Radiogenic isotopes: the case for crustal recycling on a near-steady-state no-continental-growth Earth. Philos Trans R Soc London A301:443?472

3. Arnbom JO (1980) The metamorphism of the Seve Nappes at Åreskutan, Swedish Caledonides. Geol Foeren Stockholm Foerh 102:359?371

4. Claesson S (1982) Caledonian metamorphism of Proterozoic Seve rocks on Mt Åreskutan, southern Swedish Caledonides. Geol Foeren Stockholm Foerh 103:291?304

5. Corfu F (1980) U-Pb and Rb-Sr systematics in a polyorogenic segment of the Precambrian shield, central southern Norway. Lithos 13:305?323

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