BERINGOVSKY BASIN COALS METAMORPHISM

Main type of coals metamorphism in Beringovsky basin is stated to be regional. According to the degree of carbonification coals of the basin change from long-flame to fat (the I-III stages of a metamorphism). A degree of a metamorphism of deposited coals increases with stratigraphic depth and with i...

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Main Author: G. A. Fandyushkin
Format: Article
Language:Russian
Published: Sergo Ordzhonikidze Russian State University for Geological Prospecting 2016-08-01
Series:Известия высших учебных заведений: Геология и разведка
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Online Access:https://www.geology-mgri.ru/jour/article/view/157
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author G. A. Fandyushkin
author_facet G. A. Fandyushkin
author_sort G. A. Fandyushkin
collection DOAJ
description Main type of coals metamorphism in Beringovsky basin is stated to be regional. According to the degree of carbonification coals of the basin change from long-flame to fat (the I-III stages of a metamorphism). A degree of a metamorphism of deposited coals increases with stratigraphic depth and with increase of the thicknesses of strata covering them. The most metamorphosed coals are dated to the places of the greatest deileciions, the least metamorphosed - to the consedementation raisings. The area of distribution of the coked coals in the deposit is specified. A degree of a metamorphism of the coals in the Beringovsky basin was studied mainly on the basis of the reflective ability of a vitrinit (RAV)
format Article
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institution DOAJ
issn 0016-7762
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language Russian
publishDate 2016-08-01
publisher Sergo Ordzhonikidze Russian State University for Geological Prospecting
record_format Article
series Известия высших учебных заведений: Геология и разведка
spelling doaj-art-64a15eb7b7ee40ab9983ba3e07aabfe72025-08-20T02:49:26ZrusSergo Ordzhonikidze Russian State University for Geological ProspectingИзвестия высших учебных заведений: Геология и разведка0016-77622618-87082016-08-0104374210.32454/0016-7762-2016-4-37-42157BERINGOVSKY BASIN COALS METAMORPHISMG. A. Fandyushkin0Закрытое акционерное общество «Северо-Тихоокеанская угольная компания»Main type of coals metamorphism in Beringovsky basin is stated to be regional. According to the degree of carbonification coals of the basin change from long-flame to fat (the I-III stages of a metamorphism). A degree of a metamorphism of deposited coals increases with stratigraphic depth and with increase of the thicknesses of strata covering them. The most metamorphosed coals are dated to the places of the greatest deileciions, the least metamorphosed - to the consedementation raisings. The area of distribution of the coked coals in the deposit is specified. A degree of a metamorphism of the coals in the Beringovsky basin was studied mainly on the basis of the reflective ability of a vitrinit (RAV)https://www.geology-mgri.ru/jour/article/view/157coal basincarboniferous regioncarboniferous hollowmetamorphism of coalsbranded composition of coalscatagenesis of rocksreflective ability of a vitrinit
spellingShingle G. A. Fandyushkin
BERINGOVSKY BASIN COALS METAMORPHISM
Известия высших учебных заведений: Геология и разведка
coal basin
carboniferous region
carboniferous hollow
metamorphism of coals
branded composition of coals
catagenesis of rocks
reflective ability of a vitrinit
title BERINGOVSKY BASIN COALS METAMORPHISM
title_full BERINGOVSKY BASIN COALS METAMORPHISM
title_fullStr BERINGOVSKY BASIN COALS METAMORPHISM
title_full_unstemmed BERINGOVSKY BASIN COALS METAMORPHISM
title_short BERINGOVSKY BASIN COALS METAMORPHISM
title_sort beringovsky basin coals metamorphism
topic coal basin
carboniferous region
carboniferous hollow
metamorphism of coals
branded composition of coals
catagenesis of rocks
reflective ability of a vitrinit
url https://www.geology-mgri.ru/jour/article/view/157
work_keys_str_mv AT gafandyushkin beringovskybasincoalsmetamorphism