Zircon from the East Orebody of the Bayan Obo Fe–Nb–REE deposit, China, and SHRIMP ages for carbonatite-related magmatism and REE mineralization events-Reference-Cited by-同舟云学术

Zircon from the East Orebody of the Bayan Obo Fe–Nb–REE deposit, China, and SHRIMP ages for carbonatite-related magmatism and REE mineralization events

Published:2014-08 Issue:2 Volume:168 Page:
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Campbell L. S.,Compston W.,Sircombe K. N.,Wilkinson C. C.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/article/10.1007/s00410-014-1041-3/fulltext.html

Reference97 articles.

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3. Blundy J, Dalton J (2000) Experimental comparison of trace element partitioning between clinopyroxene and melt in carbonate and silicate systems, and implications for mantle metasomatism. Contrib Mineral Petrol 139(3):356–371. doi: 10.1007/s004100000139

4. Blundy J, Wood B (2003) Partitioning of trace elements between crystals and melts. Earth Planet Sci Lett 210:383–397. doi: 10.1016/S0012-821X(03)00129-8

5. Boynton WV (1984) Geochemistry of the rare earth elements: meteorite studies. In: Henderson P (ed) Rare earth element geochemistry. Elsevier, Amsterdam, pp 63–114

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