Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Y–REE Mineralization in Biotite–Arfvedsonite Granites of the Katugin Rare-Metal Deposit, Transbaikalia, Russia. / Starikova, A. E.; Sklyarov, E. V.; Sharygin, V. V.
в: Doklady Earth Sciences, Том 487, № 1, 01.07.2019, стр. 800-803.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Y–REE Mineralization in Biotite–Arfvedsonite Granites of the Katugin Rare-Metal Deposit, Transbaikalia, Russia
AU - Starikova, A. E.
AU - Sklyarov, E. V.
AU - Sharygin, V. V.
N1 - Publisher Copyright: © 2019, Pleiades Publishing, Ltd.
PY - 2019/7/1
Y1 - 2019/7/1
N2 - Abstract: This paper reports on the results of studies of the carbonate–fluoride isolations with extremely high Y and REE concentrations from biotite–arfvedsonite granite of the Katugin rare metal deposit. We obtained the chemical data on that minerals that compose these isolations—gagarinite-(Y), tveitite-(Y), fluocerite-(Ce), bastnaesite, and fluornatropyrochlore. A carbonate–fluoride globule with a well-preserved crystallization order was revealed in quartz of the host granite. This finding might be evidence of silicate–fluorine immiscibility suggested before for the Y–REE isolations in the Katugin granites. We assumed that the fluoride melt occurred at the magmatic stage of the formation of biotite–arfvedsonite granite, which resulted in depletion of the host granite with fluorine and the redistribution of the REE and Y in the fluoride salt melt.
AB - Abstract: This paper reports on the results of studies of the carbonate–fluoride isolations with extremely high Y and REE concentrations from biotite–arfvedsonite granite of the Katugin rare metal deposit. We obtained the chemical data on that minerals that compose these isolations—gagarinite-(Y), tveitite-(Y), fluocerite-(Ce), bastnaesite, and fluornatropyrochlore. A carbonate–fluoride globule with a well-preserved crystallization order was revealed in quartz of the host granite. This finding might be evidence of silicate–fluorine immiscibility suggested before for the Y–REE isolations in the Katugin granites. We assumed that the fluoride melt occurred at the magmatic stage of the formation of biotite–arfvedsonite granite, which resulted in depletion of the host granite with fluorine and the redistribution of the REE and Y in the fluoride salt melt.
KW - AGE
KW - CRYOLITE
KW - GENESIS
UR - http://www.scopus.com/inward/record.url?scp=85071495826&partnerID=8YFLogxK
U2 - 10.1134/S1028334X19070080
DO - 10.1134/S1028334X19070080
M3 - Article
AN - SCOPUS:85071495826
VL - 487
SP - 800
EP - 803
JO - Doklady Earth Sciences
JF - Doklady Earth Sciences
SN - 1028-334X
IS - 1
ER -
ID: 21452182