Residence and redistribution of REE, Y, Zr, Th and U during granulite-facies metamorphism: behaviour of accessory and major phases in peraluminous granulites of central Spain-Reference-Cited by-同舟云学术

Residence and redistribution of REE, Y, Zr, Th and U during granulite-facies metamorphism: behaviour of accessory and major phases in peraluminous granulites of central Spain

Published:2003-10 Issue:3-4 Volume:200 Page:293-323
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Villaseca C.,Martı́n Romera C.,De la Rosa J.,Barbero L.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference58 articles.

1. Granulite-facies metamorphism in the Anatectic Complex of Toledo, Spain: late Hercynian tectonic evolution by crustal extension;Barbero;J. Geol. Soc. (Lond.),1995

2. Implications of U–Pb monazite ages from syn-orogenic granites of the Anatectic Complex of Toledo (Spain) in the evolution of the central part of the Hercynian Iberian Belt;Barbero;Doc. BRGM,1999

3. Eclogite facies relics in metabasites from the Sierra de Guadarrama (Spanish Central System): P–T estimations and implications for the Hercynian evolution;Barbero;Mineral. Mag.,2000

4. Geochemical and isotopic disequilibrium in crustal melting: an insight from anatectic granitoids from Toledo, Spain;Barbero;J. Geophys. Res.,1995

5. Residence of REE, Y, Th and U in granites and crustal protoliths: implications for the chemistry of crustal melts;Bea;J. Petrol.,1996

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