High to ultrahigh temperature contact metamorphism and dry partial melting of the Tasiuyak paragneiss, Northern Labrador-Reference-Cited by-同舟云学术

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High to ultrahigh temperature contact metamorphism and dry partial melting of the Tasiuyak paragneiss, Northern Labrador

Published:2014-04-17 Issue:6 Volume:32 Page:535-555
ISSN:0263-4929
Container-title:Journal of Metamorphic Geology
language:en
Short-container-title:J. Meta. Geol.

Author:

Mitchell R. K.¹,Indares A.²,Ryan B.³

Affiliation:

1. Earth Science Department; Carleton University; 1125 Colonel By Drive Ottawa ON Canada K1S 5B6

2. Department of Earth Sciences; Memorial University of Newfoundland and Labrador; P.O. Box 4200 St. John's NL Canada A1C 5S7

3. Department of Natural Resources; Geological Survey of Newfoundland and Labrador; Box 8700 St. John's NL Canada A1B 4J6

Funder

National Science and Engineering Research Council

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/jmg.12086/fullpdf

Reference79 articles.

1. Multistage progressive evolution of rare osumilite-bearing assemblages preserved in ultrahigh-temperature granulites from In Ouzzal (Hoggar, Algeria);Adjerid;Journal of Metamorphic Geology,2013

2. Osumilite-bearing granulites in the eastern Grenville Province, eastern Labrador, Canada: mineral parageneses and metamorphic conditions;Arima;Journal of Petrology,1991

3. Cordierite-K-feldspar-quartz-orthopyroxene symplectite from southern Algeria: new evidence for osumilite in high grade metamorphic rocks;Audibert;Mineralogical Magazine,1993

4. Diffusion-controlled biotite breakdown reaction textures at the solid/liquid transition in the continental crust;Barbey;Contributions to Mineralogy and Petrology,2003

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