Major and trace element composition of melts from the Gorely volcanic center, southern Kamchatka ...

Melt inclusions in olivine and plagioclase phenocrysts from rocks (magnesian basalt, basaltic andesite, andesite, ignimbrite, and dacite) of various age from the Gorely volcanic center, southern Kamchatka, were studied by means of their homogenization and by analyzing the glasses in 100 melt inclusi...

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Main Authors: Tolstykh, M L, Naumov, V B, Gavrilenko, M G, Ozerov, AYu, Kononkova, N N
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2012
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.793071
https://doi.pangaea.de/10.1594/PANGAEA.793071
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author Tolstykh, M L
Naumov, V B
Gavrilenko, M G
Ozerov, AYu
Kononkova, N N
author_facet Tolstykh, M L
Naumov, V B
Gavrilenko, M G
Ozerov, AYu
Kononkova, N N
author_sort Tolstykh, M L
collection DataCite
description Melt inclusions in olivine and plagioclase phenocrysts from rocks (magnesian basalt, basaltic andesite, andesite, ignimbrite, and dacite) of various age from the Gorely volcanic center, southern Kamchatka, were studied by means of their homogenization and by analyzing the glasses in 100 melt inclusions on an electron microprobe and 24 inclusions on an ion probe. The SiO2 concentrations of the melts vary within a broad range of 45-74 wt%, as also are the concentrations of other major components. According to their SiO2, Na2O, K2O, TiO2, and P2O5 concentrations, the melts are classified into seven groups. The mafic melts (45-53 wt% SiO2) comprise the following varieties: potassic (on average 4.2 wt% K2O, 1.7 wt% Na2O, 1.0 wt% TiO2, and 0.20 wt% P2O5), sodic (3.2% Na2O, 1.1% K2O, 1.1% TiO2, and 0.40% P2O5), and titaniferous with high P2O5 concentrations (2.2% TiO2, 1.1% P2O5, 3.8% Na2O, and 3.0% K2O). The melts of intermediate composition (53-64% SiO2) also include potassic (5.6% K2O, 3.4% Na2O, 1.0% TiO2, and ... : Supplement to: Tolstykh, M L; Naumov, V B; Gavrilenko, M G; Ozerov, AYu; Kononkova, N N (2012): Chemical composition, volatile components, and trace elements in the melts of the Gorely volcanic center, southern Kamchatka: Evidence from inclusions in minerals. Geochemistry International, 50(6), 522-550 ...
format Article in Journal/Newspaper
genre Kamchatka
genre_facet Kamchatka
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op_doi https://doi.org/10.1594/pangaea.79307110.1134/s0016702912060079
op_relation https://dx.doi.org/10.1134/s0016702912060079
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
publishDate 2012
publisher PANGAEA
record_format openpolar
spelling ftdatacite:10.1594/pangaea.793071 2025-01-16T22:48:23+00:00 Major and trace element composition of melts from the Gorely volcanic center, southern Kamchatka ... Tolstykh, M L Naumov, V B Gavrilenko, M G Ozerov, AYu Kononkova, N N 2012 application/zip https://dx.doi.org/10.1594/pangaea.793071 https://doi.pangaea.de/10.1594/PANGAEA.793071 en eng PANGAEA https://dx.doi.org/10.1134/s0016702912060079 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Archive of Ocean Data ARCOD article Collection Supplementary Publication Series of Datasets 2012 ftdatacite https://doi.org/10.1594/pangaea.79307110.1134/s0016702912060079 2024-08-01T11:00:37Z Melt inclusions in olivine and plagioclase phenocrysts from rocks (magnesian basalt, basaltic andesite, andesite, ignimbrite, and dacite) of various age from the Gorely volcanic center, southern Kamchatka, were studied by means of their homogenization and by analyzing the glasses in 100 melt inclusions on an electron microprobe and 24 inclusions on an ion probe. The SiO2 concentrations of the melts vary within a broad range of 45-74 wt%, as also are the concentrations of other major components. According to their SiO2, Na2O, K2O, TiO2, and P2O5 concentrations, the melts are classified into seven groups. The mafic melts (45-53 wt% SiO2) comprise the following varieties: potassic (on average 4.2 wt% K2O, 1.7 wt% Na2O, 1.0 wt% TiO2, and 0.20 wt% P2O5), sodic (3.2% Na2O, 1.1% K2O, 1.1% TiO2, and 0.40% P2O5), and titaniferous with high P2O5 concentrations (2.2% TiO2, 1.1% P2O5, 3.8% Na2O, and 3.0% K2O). The melts of intermediate composition (53-64% SiO2) also include potassic (5.6% K2O, 3.4% Na2O, 1.0% TiO2, and ... : Supplement to: Tolstykh, M L; Naumov, V B; Gavrilenko, M G; Ozerov, AYu; Kononkova, N N (2012): Chemical composition, volatile components, and trace elements in the melts of the Gorely volcanic center, southern Kamchatka: Evidence from inclusions in minerals. Geochemistry International, 50(6), 522-550 ... Article in Journal/Newspaper Kamchatka DataCite
spellingShingle Archive of Ocean Data ARCOD
Tolstykh, M L
Naumov, V B
Gavrilenko, M G
Ozerov, AYu
Kononkova, N N
Major and trace element composition of melts from the Gorely volcanic center, southern Kamchatka ...
title Major and trace element composition of melts from the Gorely volcanic center, southern Kamchatka ...
title_full Major and trace element composition of melts from the Gorely volcanic center, southern Kamchatka ...
title_fullStr Major and trace element composition of melts from the Gorely volcanic center, southern Kamchatka ...
title_full_unstemmed Major and trace element composition of melts from the Gorely volcanic center, southern Kamchatka ...
title_short Major and trace element composition of melts from the Gorely volcanic center, southern Kamchatka ...
title_sort major and trace element composition of melts from the gorely volcanic center, southern kamchatka ...
topic Archive of Ocean Data ARCOD
topic_facet Archive of Ocean Data ARCOD
url https://dx.doi.org/10.1594/pangaea.793071
https://doi.pangaea.de/10.1594/PANGAEA.793071