CRYSTALLIZATION CONDITIONS OF OLIVINE IN DUNITES THE GULI MASSIF, SIBERIAN PLATFORM

Crystallization conditions of olivine in dunites of the Guli massif (Siberian Platform) are established using petrological, geochemical, mineralogical and thermobarogeochemical methods. The formation of olivine and chromite from picrite-meimechite ultramafic magmas was followed by the fractionation...

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Main Authors: V.A. Simonov, A.V. Kotlyarov, V.V. Sharygin, Yu.R. Vasiliev
Format: Article
Language:English
Published: South Urals Federal Research Center of Mineralogy and Geoecology UB RAS 2024-03-01
Series:Минералогия
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Online Access:https://journal.mineralogy.ru/wp-content/uploads/2024/04/2024_10_1_2.pdf
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author V.A. Simonov
A.V. Kotlyarov
V.V. Sharygin
Yu.R. Vasiliev
author_facet V.A. Simonov
A.V. Kotlyarov
V.V. Sharygin
Yu.R. Vasiliev
author_sort V.A. Simonov
collection DOAJ
description Crystallization conditions of olivine in dunites of the Guli massif (Siberian Platform) are established using petrological, geochemical, mineralogical and thermobarogeochemical methods. The formation of olivine and chromite from picrite-meimechite ultramafic magmas was followed by the fractionation of clinopyroxenes from basaltic systems with the formation of residual high-alkaline melts. The calculations in PETROLOG and COMAGMAT programs based on the compositions of inclusions and minerals, as well as using olivine-spinel geothermometer, showed that a magmatic system, which was responsible for the formation of dunites of the Guli massif, evolved during the crystallization of olivine in a wide temperature range of 1520–1250 °C in a magma chamber at a depth of about 17 km.
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id doaj-art-03547e812ff14079b23f310949a75083
institution Kabale University
issn 2313-545X
2782-2044
language English
publishDate 2024-03-01
publisher South Urals Federal Research Center of Mineralogy and Geoecology UB RAS
record_format Article
series Минералогия
spelling doaj-art-03547e812ff14079b23f310949a750832025-02-06T11:58:21ZengSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASМинералогия2313-545X2782-20442024-03-01101163110.35597/2313-545X-2024-10-1-2CRYSTALLIZATION CONDITIONS OF OLIVINE IN DUNITES THE GULI MASSIF, SIBERIAN PLATFORMV.A. Simonov0A.V. Kotlyarov1V.V. Sharygin2Yu.R. Vasiliev3Institute of Geology and Mineralogy SB RASInstitute of Geology and Mineralogy SB RASInstitute of Geology and Mineralogy SB RASInstitute of Geology and Mineralogy SB RASCrystallization conditions of olivine in dunites of the Guli massif (Siberian Platform) are established using petrological, geochemical, mineralogical and thermobarogeochemical methods. The formation of olivine and chromite from picrite-meimechite ultramafic magmas was followed by the fractionation of clinopyroxenes from basaltic systems with the formation of residual high-alkaline melts. The calculations in PETROLOG and COMAGMAT programs based on the compositions of inclusions and minerals, as well as using olivine-spinel geothermometer, showed that a magmatic system, which was responsible for the formation of dunites of the Guli massif, evolved during the crystallization of olivine in a wide temperature range of 1520–1250 °C in a magma chamber at a depth of about 17 km.https://journal.mineralogy.ru/wp-content/uploads/2024/04/2024_10_1_2.pdfolivinecrystallization conditionsmelt inclusionsduniteguli massifsiberian platform
spellingShingle V.A. Simonov
A.V. Kotlyarov
V.V. Sharygin
Yu.R. Vasiliev
CRYSTALLIZATION CONDITIONS OF OLIVINE IN DUNITES THE GULI MASSIF, SIBERIAN PLATFORM
Минералогия
olivine
crystallization conditions
melt inclusions
dunite
guli massif
siberian platform
title CRYSTALLIZATION CONDITIONS OF OLIVINE IN DUNITES THE GULI MASSIF, SIBERIAN PLATFORM
title_full CRYSTALLIZATION CONDITIONS OF OLIVINE IN DUNITES THE GULI MASSIF, SIBERIAN PLATFORM
title_fullStr CRYSTALLIZATION CONDITIONS OF OLIVINE IN DUNITES THE GULI MASSIF, SIBERIAN PLATFORM
title_full_unstemmed CRYSTALLIZATION CONDITIONS OF OLIVINE IN DUNITES THE GULI MASSIF, SIBERIAN PLATFORM
title_short CRYSTALLIZATION CONDITIONS OF OLIVINE IN DUNITES THE GULI MASSIF, SIBERIAN PLATFORM
title_sort crystallization conditions of olivine in dunites the guli massif siberian platform
topic olivine
crystallization conditions
melt inclusions
dunite
guli massif
siberian platform
url https://journal.mineralogy.ru/wp-content/uploads/2024/04/2024_10_1_2.pdf
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