Diffusion controlled growth of pyroxene-bearing margins on amphibolite bands in the granulite facies of Rogaland (Southwestern Norway): implications for granulite formation-Reference-Cited by-同舟云学术

Diffusion controlled growth of pyroxene-bearing margins on amphibolite bands in the granulite facies of Rogaland (Southwestern Norway): implications for granulite formation

Published:1993-06 Issue:2 Volume:114 Page:203-220
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contr. Mineral. and Petrol.

Author:

Vander Auwera J.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF00307756.pdf

Reference61 articles.

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2. Barbey P, Cuney M (1982) K, Rb, Sr, Ba, U and Th geochemistry of the Lapland granulites (Fennoscandia): LILE fractionation controlling factors. Contrib Mineral Petrol 81: 304?316

3. Barbey P, Bertrand JM, Angoua S, Dautel D (1989) Petrology and U/Pb geochronology of the Telohat migmatites, Aleksod, Central Hoggar, Algeria. Contrib Mineral Petrol 101: 207?219

4. Bingen B (1989) Geochemistry of Sveconorwegian augen gneisses from SW Norway at the amphibolite-granulite-facies transition. Nor Geol Tidsskr 69: 177?189

5. Bingen B, Demaiffe D, Hertogen J (1990) Evolution of feldspars at the amphibolite-granulite facies transition in augen gneisses (SW Norway): geochemistry and Sr isotopes. Contrib Mineral Petrol 105: 275?288

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