CRYSTALLIZATION CONDITIONS OF PLAGIOCLASE IN VOLCANIC COMPLEXES OF SULAWESI ISLAND, PACIFIC OCEAN

Mineralogical and thermobarogeochemical studies allowed us to reveal the crystallization conditions of plagioclase in volcanic complexes of Sulawesi Island (Pacific Ocean). The composition of plagioclase indicates the presence of three types of melts, which were involved in the formation of plagiocl...

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Main Authors: A.V. Kotlyarov, N.V. Dmitrieva, V.A. Simonov, I.Yu. Safonova, N.S. Karmanov, I.R. Nizametdinov
Format: Article
Language:English
Published: South Urals Federal Research Center of Mineralogy and Geoecology UB RAS 2023-03-01
Series:Минералогия
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Online Access:https://journal.mineralogy.ru/wp-content/uploads/2023/04/2023_9_1_4.pdf
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author A.V. Kotlyarov
N.V. Dmitrieva
V.A. Simonov
I.Yu. Safonova
N.S. Karmanov
I.R. Nizametdinov
author_facet A.V. Kotlyarov
N.V. Dmitrieva
V.A. Simonov
I.Yu. Safonova
N.S. Karmanov
I.R. Nizametdinov
author_sort A.V. Kotlyarov
collection DOAJ
description Mineralogical and thermobarogeochemical studies allowed us to reveal the crystallization conditions of plagioclase in volcanic complexes of Sulawesi Island (Pacific Ocean). The composition of plagioclase indicates the presence of three types of melts, which were involved in the formation of plagioclase phenocrysts in basalts, andesites and dacites, as well as crystallites in the groundmass of andesites and dacites. The analysis of glasses of heated melt inclusions in plagioclase indicates the involvement of two contrasting melts (mafic and felsic) in crystallization of phenocrysts. At the final stages of the volcanic process, plagioclase in matrix of andesites and dacites formed from another felsic melts with maximum alkali content. The presence of primary syngenetic melt and fluid inclusions in plagioclase phenocrysts indicates the phase separation of felsic magmas, which led to the crystallization of feldspar phenocrysts of different composition during the formation of dacites. Computational modeling in a program of (Putirka, 2008) based on the composition of plagioclases, glasses of heated inclusions and glasses from the groundmass allowed us to estimate the crystallization temperatures of feldspar phenocrysts in basalt (1160–1120 ºС), andesite (930–890 ºС) and dacite (1035–970 ºС), as well as the feldspar microcrystals in the groundmass of andesite (875–810 ºС) and dacite (900–865 ºС).
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institution Kabale University
issn 2313-545X
2782-2044
language English
publishDate 2023-03-01
publisher South Urals Federal Research Center of Mineralogy and Geoecology UB RAS
record_format Article
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spelling doaj-art-2075f739f8d7493ea569b6b93131d7802025-02-07T10:55:20ZengSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASМинералогия2313-545X2782-20442023-03-0191607810.35597/2313-545X-2023-9-1-4CRYSTALLIZATION CONDITIONS OF PLAGIOCLASE IN VOLCANIC COMPLEXES OF SULAWESI ISLAND, PACIFIC OCEANA.V. Kotlyarov0N.V. Dmitrieva1V.A. Simonov2I.Yu. Safonova3N.S. Karmanov4I.R. Nizametdinov5Institute of Geology and Mineralogy SB RASInstitute of Geology and Mineralogy SB RASInstitute of Geology and Mineralogy SB RASInstitute of Geology and Mineralogy SB RASInstitute of Geology and Mineralogy SB RASInstitute of Geology and Mineralogy SB RASMineralogical and thermobarogeochemical studies allowed us to reveal the crystallization conditions of plagioclase in volcanic complexes of Sulawesi Island (Pacific Ocean). The composition of plagioclase indicates the presence of three types of melts, which were involved in the formation of plagioclase phenocrysts in basalts, andesites and dacites, as well as crystallites in the groundmass of andesites and dacites. The analysis of glasses of heated melt inclusions in plagioclase indicates the involvement of two contrasting melts (mafic and felsic) in crystallization of phenocrysts. At the final stages of the volcanic process, plagioclase in matrix of andesites and dacites formed from another felsic melts with maximum alkali content. The presence of primary syngenetic melt and fluid inclusions in plagioclase phenocrysts indicates the phase separation of felsic magmas, which led to the crystallization of feldspar phenocrysts of different composition during the formation of dacites. Computational modeling in a program of (Putirka, 2008) based on the composition of plagioclases, glasses of heated inclusions and glasses from the groundmass allowed us to estimate the crystallization temperatures of feldspar phenocrysts in basalt (1160–1120 ºС), andesite (930–890 ºС) and dacite (1035–970 ºС), as well as the feldspar microcrystals in the groundmass of andesite (875–810 ºС) and dacite (900–865 ºС).https://journal.mineralogy.ru/wp-content/uploads/2023/04/2023_9_1_4.pdfcrystallization conditionsplagioclasemelt inclusionssulawesi islandpacific ocean
spellingShingle A.V. Kotlyarov
N.V. Dmitrieva
V.A. Simonov
I.Yu. Safonova
N.S. Karmanov
I.R. Nizametdinov
CRYSTALLIZATION CONDITIONS OF PLAGIOCLASE IN VOLCANIC COMPLEXES OF SULAWESI ISLAND, PACIFIC OCEAN
Минералогия
crystallization conditions
plagioclase
melt inclusions
sulawesi island
pacific ocean
title CRYSTALLIZATION CONDITIONS OF PLAGIOCLASE IN VOLCANIC COMPLEXES OF SULAWESI ISLAND, PACIFIC OCEAN
title_full CRYSTALLIZATION CONDITIONS OF PLAGIOCLASE IN VOLCANIC COMPLEXES OF SULAWESI ISLAND, PACIFIC OCEAN
title_fullStr CRYSTALLIZATION CONDITIONS OF PLAGIOCLASE IN VOLCANIC COMPLEXES OF SULAWESI ISLAND, PACIFIC OCEAN
title_full_unstemmed CRYSTALLIZATION CONDITIONS OF PLAGIOCLASE IN VOLCANIC COMPLEXES OF SULAWESI ISLAND, PACIFIC OCEAN
title_short CRYSTALLIZATION CONDITIONS OF PLAGIOCLASE IN VOLCANIC COMPLEXES OF SULAWESI ISLAND, PACIFIC OCEAN
title_sort crystallization conditions of plagioclase in volcanic complexes of sulawesi island pacific ocean
topic crystallization conditions
plagioclase
melt inclusions
sulawesi island
pacific ocean
url https://journal.mineralogy.ru/wp-content/uploads/2023/04/2023_9_1_4.pdf
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