Research output: Contribution to journal › Article › peer-review
An X-ray Diffraction Method for Estimating the Temperature of Vesuvianite Crystallization. / Panikorovskii, T.L.; Yakovenchuk, V.N.; Krivovichev, S.
In: Geology of Ore Deposits, Vol. 66, No. 7, 2024, p. 1022-1033.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - An X-ray Diffraction Method for Estimating the Temperature of Vesuvianite Crystallization
AU - Panikorovskii, T.L.
AU - Yakovenchuk, V.N.
AU - Krivovichev, S.
N1 - Export Date: 01 November 2025; Cited By: 0; Correspondence Address: T.L. Panikorovskii; Kola Science Centre, Russian Academy of Sciences, Apatity, 184209, Russian Federation; email: taras.panikorovskii@ksc.ru
PY - 2024
Y1 - 2024
N2 - Abstract: The article provides an empirical method for using the number of violating reflections for the P4/nnc space group to estimate the formation temperature of different polytypes (P4/nnc, P4/n, and P4nc) of vesuvianite group minerals. For this purpose, a statistical approach based on an instrumentally investigated 197 samples of vesuvianite group minerals was used. As an example, the results of a study of a number of vesuvianite group samples from skarnoids of the Kovdor alkaline massif are considered. Crystal and chemical limitations of the proposed approach that are associated with the chemical composition and kinetics of crystallization of vesuvianite group minerals are also discussed. © 2025 Elsevier B.V., All rights reserved.
AB - Abstract: The article provides an empirical method for using the number of violating reflections for the P4/nnc space group to estimate the formation temperature of different polytypes (P4/nnc, P4/n, and P4nc) of vesuvianite group minerals. For this purpose, a statistical approach based on an instrumentally investigated 197 samples of vesuvianite group minerals was used. As an example, the results of a study of a number of vesuvianite group samples from skarnoids of the Kovdor alkaline massif are considered. Crystal and chemical limitations of the proposed approach that are associated with the chemical composition and kinetics of crystallization of vesuvianite group minerals are also discussed. © 2025 Elsevier B.V., All rights reserved.
KW - crystalline structure
KW - formation temperature
KW - geothermometer
KW - Kovdor massif
KW - vesuvianite
KW - Alkalinity
KW - Hydrogeology
KW - Miocene
KW - Crystalline structure
KW - Empirical method
KW - Formation temperature
KW - Geothermometers
KW - Polytypes
KW - Space Groups
KW - Statistical approach
KW - Vesuvianite
KW - X-ray diffraction method
KW - Crystallization kinetics
KW - crystal structure
KW - crystallization
KW - geothermometry
KW - temperature
KW - X-ray diffraction
U2 - 10.1134/S1075701524700156
DO - 10.1134/S1075701524700156
M3 - статья
VL - 66
SP - 1022
EP - 1033
JO - Geology of Ore Deposits
JF - Geology of Ore Deposits
SN - 1075-7015
IS - 7
ER -
ID: 143367849