RELATIVE AGE OF ACCESSORY MINERALS IN PEGMATITES OF THE ILMENY MOUNTAINS, SOUTH URALS

Effective retrospective modeling of mineral formation in natural systems should take into account all minerals – rock-forming, secondary in abundance and accessory. In the Ilmeny Mountains (South Urals), the ontogeny of pegmatite bodies (granitic, syenitic, carbonatite, and ultramafic) is complex in...

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Main Author: V.A. Popov
Format: Article
Language:English
Published: South Urals Federal Research Center of Mineralogy and Geoecology UB RAS 2021-03-01
Series:Минералогия
Subjects:
Online Access:https://journal.mineralogy.ru/wp-content/uploads/2021/03/2021_7_1_2.pdf
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author V.A. Popov
author_facet V.A. Popov
author_sort V.A. Popov
collection DOAJ
description Effective retrospective modeling of mineral formation in natural systems should take into account all minerals – rock-forming, secondary in abundance and accessory. In the Ilmeny Mountains (South Urals), the ontogeny of pegmatite bodies (granitic, syenitic, carbonatite, and ultramafic) is complex in time and space. Using several examples, the relative age of accessory minerals in aggregates of rock-forming minerals is considered against the background of a general evolution of formation of pegmatite fields.
format Article
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institution Kabale University
issn 2313-545X
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language English
publishDate 2021-03-01
publisher South Urals Federal Research Center of Mineralogy and Geoecology UB RAS
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spelling doaj-art-2b56e8f813bd4f44bacedb04f17ccf382025-02-12T08:51:56ZengSouth Urals Federal Research Center of Mineralogy and Geoecology UB RASМинералогия2313-545X2782-20442021-03-0171233910.35597/2313-545X-2021-7-1-2RELATIVE AGE OF ACCESSORY MINERALS IN PEGMATITES OF THE ILMENY MOUNTAINS, SOUTH URALSV.A. Popov0South Urals Federal Research Center of Mineralogy and Geoecology UB RASEffective retrospective modeling of mineral formation in natural systems should take into account all minerals – rock-forming, secondary in abundance and accessory. In the Ilmeny Mountains (South Urals), the ontogeny of pegmatite bodies (granitic, syenitic, carbonatite, and ultramafic) is complex in time and space. Using several examples, the relative age of accessory minerals in aggregates of rock-forming minerals is considered against the background of a general evolution of formation of pegmatite fields.https://journal.mineralogy.ru/wp-content/uploads/2021/03/2021_7_1_2.pdfpegmatitesaccessory mineralsontogenesisilmeny mountains
spellingShingle V.A. Popov
RELATIVE AGE OF ACCESSORY MINERALS IN PEGMATITES OF THE ILMENY MOUNTAINS, SOUTH URALS
Минералогия
pegmatites
accessory minerals
ontogenesis
ilmeny mountains
title RELATIVE AGE OF ACCESSORY MINERALS IN PEGMATITES OF THE ILMENY MOUNTAINS, SOUTH URALS
title_full RELATIVE AGE OF ACCESSORY MINERALS IN PEGMATITES OF THE ILMENY MOUNTAINS, SOUTH URALS
title_fullStr RELATIVE AGE OF ACCESSORY MINERALS IN PEGMATITES OF THE ILMENY MOUNTAINS, SOUTH URALS
title_full_unstemmed RELATIVE AGE OF ACCESSORY MINERALS IN PEGMATITES OF THE ILMENY MOUNTAINS, SOUTH URALS
title_short RELATIVE AGE OF ACCESSORY MINERALS IN PEGMATITES OF THE ILMENY MOUNTAINS, SOUTH URALS
title_sort relative age of accessory minerals in pegmatites of the ilmeny mountains south urals
topic pegmatites
accessory minerals
ontogenesis
ilmeny mountains
url https://journal.mineralogy.ru/wp-content/uploads/2021/03/2021_7_1_2.pdf
work_keys_str_mv AT vapopov relativeageofaccessorymineralsinpegmatitesoftheilmenymountainssouthurals