Coefficients of distribution of REE+Y between minerals and cooling rich sulfate fluid (thermodynamic modeling)
The relevance of the work is caused by the fact that the study of the coefficients of REE+Y distribution between the minerals-concentrators of these elements and between minerals and sulfate fluids in various alkaline and weakly acidic systems makes it possible to obtain the missing parameters neces...
Main Authors: | Galina Petrovna Shironosova, Ilya Romanovich Prokopyev |
---|---|
Format: | Article |
Language: | Russian |
Published: |
Tomsk Polytechnic University
2018-11-01
|
Series: | Известия Томского политехнического университета: Инжиниринг георесурсов |
Subjects: | |
Online Access: | http://izvestiya.tpu.ru/archive/article/view/2100 |
Similar Items
-
REE+Y behavior in fluoride-chloride-sulphide-sulphate-carbonate environment at hydrothermal stages of alkaline magmatic complexes according to thermodynamic modeling
by: Galina Petrovna Shironosova, et al.
Published: (2018-01-01) -
REE+Y behavior in fluoride-chloride-sulphide-sulphate-carbonate environment at hydrothermal stages of alkaline magmatic complexes according to thermodynamic modeling
by: Galina Petrovna Shironosova, et al.
Published: (2018-01-01) -
REE-bearing minerals in Drava river sediments, Slovenia, and their potential origin
by: Aleš Šoster, et al.
Published: (2017-12-01) -
Geochemistry of Monazite within Carbonatite Related REE Deposits
by: Wei Chen, et al.
Published: (2017-09-01) -
Composition series on (Rees) congruences of S-acts.
by: Roghaieh Khosravi, et al.
Published: (2023-08-01)