POLYAKOV LOG COARSE GARNET OCCURRENCE IN THE SOUTH URALS

Ontogenic modeling of the origin of coarse garnet of the Polyakov log occurrence (South Urals) in a fine-grained schist sequence allowed the authors to conclude on its metasomatic growth with the replacement of chlorite aggregates. Muscovite, ilmenite, epidote, quartz and apatite remain preserved in...

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Main Authors: V.A. Popov, M.A. Rassomakhin, S.V. Kolisnichenko
Format: Article
Language:English
Published: South Urals Federal Research Center of Mineralogy and Geoecology UB RAS 2023-06-01
Series:Минералогия
Subjects:
Online Access:https://journal.mineralogy.ru/wp-content/uploads/2023/06/2023_9_2_5.pdf
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author V.A. Popov
M.A. Rassomakhin
S.V. Kolisnichenko
author_facet V.A. Popov
M.A. Rassomakhin
S.V. Kolisnichenko
author_sort V.A. Popov
collection DOAJ
description Ontogenic modeling of the origin of coarse garnet of the Polyakov log occurrence (South Urals) in a fine-grained schist sequence allowed the authors to conclude on its metasomatic growth with the replacement of chlorite aggregates. Muscovite, ilmenite, epidote, quartz and apatite remain preserved in the primary schist orientation of individuals. Accessory andesine, cobaltite, pentlandite, pyrrhotite and zircon crystallized together with garnet. The formation of coarse garnet crystals is probably related to fluctuations of supersaturation relative to garnet in areas of schists with abundant chlorite. This allows us to expect the presence of coarse garnet areas in adjacent parts of the schist sequence.
format Article
id doaj-art-11088fba9ae24f1483b869675aa03cea
institution Kabale University
issn 2313-545X
2782-2044
language English
publishDate 2023-06-01
publisher South Urals Federal Research Center of Mineralogy and Geoecology UB RAS
record_format Article
series Минералогия
spelling doaj-art-11088fba9ae24f1483b869675aa03cea2025-02-07T10:45:31ZengSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASМинералогия2313-545X2782-20442023-06-0192606610.35597/2313-545X-2023-9-2-5POLYAKOV LOG COARSE GARNET OCCURRENCE IN THE SOUTH URALSV.A. Popov0M.A. Rassomakhin1S.V. Kolisnichenko2South Urals Federal Research Center of Mineralogy and Geoecology UB RASSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASOntogenic modeling of the origin of coarse garnet of the Polyakov log occurrence (South Urals) in a fine-grained schist sequence allowed the authors to conclude on its metasomatic growth with the replacement of chlorite aggregates. Muscovite, ilmenite, epidote, quartz and apatite remain preserved in the primary schist orientation of individuals. Accessory andesine, cobaltite, pentlandite, pyrrhotite and zircon crystallized together with garnet. The formation of coarse garnet crystals is probably related to fluctuations of supersaturation relative to garnet in areas of schists with abundant chlorite. This allows us to expect the presence of coarse garnet areas in adjacent parts of the schist sequence.https://journal.mineralogy.ru/wp-content/uploads/2023/06/2023_9_2_5.pdfsouth uralsgarnetontogeny
spellingShingle V.A. Popov
M.A. Rassomakhin
S.V. Kolisnichenko
POLYAKOV LOG COARSE GARNET OCCURRENCE IN THE SOUTH URALS
Минералогия
south urals
garnet
ontogeny
title POLYAKOV LOG COARSE GARNET OCCURRENCE IN THE SOUTH URALS
title_full POLYAKOV LOG COARSE GARNET OCCURRENCE IN THE SOUTH URALS
title_fullStr POLYAKOV LOG COARSE GARNET OCCURRENCE IN THE SOUTH URALS
title_full_unstemmed POLYAKOV LOG COARSE GARNET OCCURRENCE IN THE SOUTH URALS
title_short POLYAKOV LOG COARSE GARNET OCCURRENCE IN THE SOUTH URALS
title_sort polyakov log coarse garnet occurrence in the south urals
topic south urals
garnet
ontogeny
url https://journal.mineralogy.ru/wp-content/uploads/2023/06/2023_9_2_5.pdf
work_keys_str_mv AT vapopov polyakovlogcoarsegarnetoccurrenceinthesouthurals
AT marassomakhin polyakovlogcoarsegarnetoccurrenceinthesouthurals
AT svkolisnichenko polyakovlogcoarsegarnetoccurrenceinthesouthurals