Zircon coronas around Fe–Ti oxides: a physical reference frame for metamorphic and metasomatic reactions-Reference-Cited by-同舟云学术

Zircon coronas around Fe–Ti oxides: a physical reference frame for metamorphic and metasomatic reactions

Published:2008-03-28 Issue:4 Volume:156 Page:517-527
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Austrheim Håkon,Putnis Christine V.,Engvik Ane K.,Putnis Andrew

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00410-008-0299-8.pdf

Reference42 articles.

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2. Alirezaei S, Cameron EM (2002) Mass balance gabbro–amphibolite transition, Bamble sector, Norway: implications for petrogenesis and tectonic setting of gabbros. Lithos 60:21–45

3. Arnesen N (1997) Retrograde metamorphose av Granulitt facies mangeritt, Radøy-Nordhordland. Unpublished Cand Scient Thesis, University of Oslo, 119 pp

4. Ashworth JR, Joesten R (1986) The role of mamatic reactions, differentiation and annealing in the evolution of coronitic microstructures in troctolitic gabbros from Risør, Norway––a discussion. Mineral Mag 50:469–473

5. Bingen B, Austrheim H, Whitehouse M (2001) Ilmenite as a source for zirconium during high-grade metamorphism? Textural evidence from the Caledonides of Western Norway and implications for zircon geochronology. J Petrol 42:355–375

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