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Thermodynamic modeling of REE behavior in oxidized hydrothermal fluids of high sulfate sulfur concentrations. / Shironosova, G. P.; Kolonin, G. R.; Borovikov, A. A. и др.

в: Doklady Earth Sciences, Том 469, № 2, 01.08.2016, стр. 855-859.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Shironosova, GP, Kolonin, GR, Borovikov, AA & Borisenko, AS 2016, 'Thermodynamic modeling of REE behavior in oxidized hydrothermal fluids of high sulfate sulfur concentrations', Doklady Earth Sciences, Том. 469, № 2, стр. 855-859. https://doi.org/10.1134/S1028334X16080158

APA

Shironosova, G. P., Kolonin, G. R., Borovikov, A. A., & Borisenko, A. S. (2016). Thermodynamic modeling of REE behavior in oxidized hydrothermal fluids of high sulfate sulfur concentrations. Doklady Earth Sciences, 469(2), 855-859. https://doi.org/10.1134/S1028334X16080158

Vancouver

Shironosova GP, Kolonin GR, Borovikov AA, Borisenko AS. Thermodynamic modeling of REE behavior in oxidized hydrothermal fluids of high sulfate sulfur concentrations. Doklady Earth Sciences. 2016 авг. 1;469(2):855-859. doi: 10.1134/S1028334X16080158

Author

Shironosova, G. P. ; Kolonin, G. R. ; Borovikov, A. A. и др. / Thermodynamic modeling of REE behavior in oxidized hydrothermal fluids of high sulfate sulfur concentrations. в: Doklady Earth Sciences. 2016 ; Том 469, № 2. стр. 855-859.

BibTeX

@article{95ed5ccf8aa644f5b0e9990abcdc1642,
title = "Thermodynamic modeling of REE behavior in oxidized hydrothermal fluids of high sulfate sulfur concentrations",
abstract = "Thermodynamic calculations using the HCh software were made for mineral equilibriums including REEs in the fluoride–sulfide–chloride–carbonate–sulfate–system in the presence of Na, Ca, and P with fluids of various acidities–alkalinities [11]. The obtained thermodynamic characteristics of thenardite allowed us to carry out the calculations for this phase under complicated hydrothermal conditions simulating the presence of oxidized fluids at 500–100°C and 2000–125 bar. Among other solid phases, REEs–fluorite, monazite, and REE–F–apatite were formed as CaF2–(Ln,Y)F3, LnPO4, and Ca5(PO4)3F–(Ln,Y)3(PO4)3 ideal solid solutions, respectively, where Ln is La, Ce, Pr, Nd, Sm, Eu, and Gd. Xenotime, anhydrite, elemental sulfur, and calcite were found as well.",
author = "Shironosova, {G. P.} and Kolonin, {G. R.} and Borovikov, {A. A.} and Borisenko, {A. S.}",
year = "2016",
month = aug,
day = "1",
doi = "10.1134/S1028334X16080158",
language = "English",
volume = "469",
pages = "855--859",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Thermodynamic modeling of REE behavior in oxidized hydrothermal fluids of high sulfate sulfur concentrations

AU - Shironosova, G. P.

AU - Kolonin, G. R.

AU - Borovikov, A. A.

AU - Borisenko, A. S.

PY - 2016/8/1

Y1 - 2016/8/1

N2 - Thermodynamic calculations using the HCh software were made for mineral equilibriums including REEs in the fluoride–sulfide–chloride–carbonate–sulfate–system in the presence of Na, Ca, and P with fluids of various acidities–alkalinities [11]. The obtained thermodynamic characteristics of thenardite allowed us to carry out the calculations for this phase under complicated hydrothermal conditions simulating the presence of oxidized fluids at 500–100°C and 2000–125 bar. Among other solid phases, REEs–fluorite, monazite, and REE–F–apatite were formed as CaF2–(Ln,Y)F3, LnPO4, and Ca5(PO4)3F–(Ln,Y)3(PO4)3 ideal solid solutions, respectively, where Ln is La, Ce, Pr, Nd, Sm, Eu, and Gd. Xenotime, anhydrite, elemental sulfur, and calcite were found as well.

AB - Thermodynamic calculations using the HCh software were made for mineral equilibriums including REEs in the fluoride–sulfide–chloride–carbonate–sulfate–system in the presence of Na, Ca, and P with fluids of various acidities–alkalinities [11]. The obtained thermodynamic characteristics of thenardite allowed us to carry out the calculations for this phase under complicated hydrothermal conditions simulating the presence of oxidized fluids at 500–100°C and 2000–125 bar. Among other solid phases, REEs–fluorite, monazite, and REE–F–apatite were formed as CaF2–(Ln,Y)F3, LnPO4, and Ca5(PO4)3F–(Ln,Y)3(PO4)3 ideal solid solutions, respectively, where Ln is La, Ce, Pr, Nd, Sm, Eu, and Gd. Xenotime, anhydrite, elemental sulfur, and calcite were found as well.

UR - http://www.scopus.com/inward/record.url?scp=84984924016&partnerID=8YFLogxK

U2 - 10.1134/S1028334X16080158

DO - 10.1134/S1028334X16080158

M3 - Article

AN - SCOPUS:84984924016

VL - 469

SP - 855

EP - 859

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 25472167