Experimental constraints on the relative stabilities of the two systems monazite-(Ce) – allanite-(Ce) – fluorapatite and xenotime-(Y) – (Y,HREE)-rich epidote – (Y,HREE)-rich fluorapatite, in high Ca and Na-Ca environments under P-T conditions of 200–1000 MPa and 450–750 °C-Reference-Cited by-同舟云学术

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Experimental constraints on the relative stabilities of the two systems monazite-(Ce) – allanite-(Ce) – fluorapatite and xenotime-(Y) – (Y,HREE)-rich epidote – (Y,HREE)-rich fluorapatite, in high Ca and Na-Ca environments under P-T conditions of 200–1000 MPa and 450–750 °C

Published:2016-09-06 Issue:2 Volume:111 Page:183-217
ISSN:0930-0708
Container-title:Mineralogy and Petrology
language:en
Short-container-title:Miner Petrol

Author:

Budzyń Bartosz,Harlov Daniel E.,Kozub-Budzyń Gabriela A.,Majka Jarosław

Funder

National Science Center of Poland (PL)

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00710-016-0464-0.pdf

Reference100 articles.

1. Ahijado A, Casillas R, Nagy G, Fernández C (2005) Sr-rich minerals in a carbonatite skarn, Fuerteventura, Canary Islands (Spain). Mineral Petrol 84:107–127

2. Åmli R, Griffin W (1975) Microprobe analysis of REE minerals using empirical correction factors. Am Mineral 60:599–606

3. Anderson JL, Bender EE (1989) Nature and origin of Proterozoic A-type granitic magmatism in the southwestern United States of America. Lithos 23:19–52

4. Andrehs G, Heinrich W (1998) Experimental determination of REE distributions between monazite and xenotime: potential for temperature-calibrated geochronology. Chem Geol 149:83–96

5. Aranovich LY, Newton RC, Manning CE (2013) Brine-assisted anatexis: experimental melting in the system haplogranite–H2O–NaCl–KCl at deep-crustal conditions. Earth Planet Sci Lett 374:111–120

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