Beryllium and Other Trace Elements in Paragneisses and Anatectic Veins of the Ultrahigh-Temperature Napier Complex, Enderby Land, East Antarctica: the Role of Sapphirine-Reference-Cited by-同舟云学术

Beryllium and Other Trace Elements in Paragneisses and Anatectic Veins of the Ultrahigh-Temperature Napier Complex, Enderby Land, East Antarctica: the Role of Sapphirine

Published:2006-01-13 Issue:5 Volume:47 Page:859-882
ISSN:1460-2415
Container-title:Journal of Petrology
language:en
Short-container-title:

Author:

GREW EDWARD S.,YATES MARTIN G.,SHEARER CHARLES K.,HAGERTY JUSTIN J.,SHERATON JOHN W.,SANDIFORD MICHAEL

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Link

http://academic.oup.com/petrology/article-pdf/47/5/859/16666430/egi098.pdf

Reference59 articles.

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2. Bea, F. (1996). Residence of REE, Y, Th and U in granites and crustal protoliths; implications for the chemistry of crustal melts. Journal of Petrology37, 521–552.

3. Bea, F. & Montero, P. (1999). Behavior of accessory phases and redistribution of Zr, REE, Y, Th, and U during metamorphism and partial melting of metapelites in the lower crust: an example from the Kinzigite Formation of Ivrea–Verbano, NW Italy. Geochimica et Cosmochimica Acta63, 1133–1153.

4. Bea, F., Pereira, M. D. & Stroh, A. (1994). Mineral/leucosome trace-element partitioning in a peraluminous migmatite (a laser ablation–ICP–MS study). Chemical Geology117, 291–312.

5. Black, L. P. & McCulloch, M. T. (1987). Evidence for isotopic equilibration of Sm–Nd whole-rock systems in early Archaean crust of Enderby Land, Antarctica. Earth and Planetary Science Letters82, 15–24.

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