Budzyń, Bartosz, Harlov, Daniel E., Kozub-Budzyń, Gabriela A., Majka, Jarosław (2017) 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. Mineralogy and Petrology, 111 (2) 183-217 doi:10.1007/s00710-016-0464-0
Reference Type | Journal (article/letter/editorial) | ||
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Title | 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 | ||
Journal | Mineralogy and Petrology | ||
Authors | Budzyń, Bartosz | Author | |
Harlov, Daniel E. | Author | ||
Kozub-Budzyń, Gabriela A. | Author | ||
Majka, Jarosław | Author | ||
Year | 2017 (April) | Volume | 111 |
Page(s) | 183-217 | Issue | 2 |
Publisher | Springer Science and Business Media LLC | ||
DOI | doi:10.1007/s00710-016-0464-0Search in ResearchGate | ||
Mindat Ref. ID | 17386 | Long-form Identifier | mindat:1:5:17386:9 |
GUID | 144a8a57-ca9a-44fc-b7cb-e2934b18e754 | ||
Full Reference | Budzyń, Bartosz, Harlov, Daniel E., Kozub-Budzyń, Gabriela A., Majka, Jarosław (2017) 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. Mineralogy and Petrology, 111 (2) 183-217 doi:10.1007/s00710-016-0464-0 | ||
Plain Text | Budzyń, Bartosz, Harlov, Daniel E., Kozub-Budzyń, Gabriela A., Majka, Jarosław (2017) 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. Mineralogy and Petrology, 111 (2) 183-217 doi:10.1007/s00710-016-0464-0 | ||
In | (2017, April) Mineralogy and Petrology Vol. 111 (2) Springer Science and Business Media LLC |
References Listed
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