КФУ. Карточка публикации. Paleogeographic causes of the formation of mineral deposits on the east of the East European platform in the Permian period

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PALEOGEOGRAPHIC CAUSES OF THE FORMATION OF MINERAL DEPOSITS ON THE EAST OF THE EAST EUROPEAN PLATFORM IN THE PERMIAN PERIOD

Форма представления

Статьи в зарубежных журналах и сборниках

Год публикации

2020

Язык

английский

Авторы, сотрудники КФУ

Балабанов Юрий Павлович, автор

Хасанов Ринат Радикович, автор

Библиографическое описание на языке оригинала

Khasanov R, Balabanov Yu., Paleogeographic causes of the formation of mineral deposits on the east of the East European platform in the Permian period//IOP Conference Series: Earth and Environmental Science. - 2020. - Vol.516, Is.1. - Art. № 012008.

Аннотация

There took place cardinal paleo- and zoogeographic changes in the second half of the Permian period and the beginning of the Triassic on the east of the East European Platform. These changes have been reflected in the geochemical features and magnetic properties of the rocks, the isotopic composition of chemical elements, the characteristics of the fauna, as well as the nature of the sediments. Permian sediments complete have an extremely complex geological structure, are characterized by a diversity of lithologic-facies composition and occurring of specific minerals, which are considered indicators of various types of lithogenesis (sulfate-carbonate rocks, coals, copper sandstones, schists, etc.). Based on lithological and paleomagnetic studies, paleogeographic reconstructions were performed. They showed that one of the factors of Perm sedimentation and related processes of the formation of ore and nonmetallic minerals are global climatic changes caused by Carboniferous-Permian glaciation.

Ключевые слова

Paleogeography, sedimentation the formation, mineral deposits, Permian, Triassic

Название журнала

IOP Conference Series: Earth and Environmental Science

URL

https://www.scopus.com/inward/record.uri?eid=2-s2.0-85087460722&doi=10.1088%2f1755-1315%2f516%2f1%2f012008&partnerID=40&md5=e1f08bd969c7d05f75b76aee61e4a06d

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https://repository.kpfu.ru/?p_id=237771

Полная запись метаданных

Поле DC	Значение	Язык
dc.contributor.author	Балабанов Юрий Павлович	ru_RU
dc.contributor.author	Хасанов Ринат Радикович	ru_RU
dc.date.accessioned	2020-01-01T00:00:00Z	ru_RU
dc.date.available	2020-01-01T00:00:00Z	ru_RU
dc.date.issued	2020	ru_RU
dc.identifier.citation	Khasanov R, Balabanov Yu., Paleogeographic causes of the formation of mineral deposits on the east of the East European platform in the Permian period//IOP Conference Series: Earth and Environmental Science. - 2020. - Vol.516, Is.1. - Art. № 012008.	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/?p_id=237771	ru_RU
dc.description.abstract	IOP Conference Series: Earth and Environmental Science	ru_RU
dc.description.abstract	There took place cardinal paleo- and zoogeographic changes in the second half of the Permian period and the beginning of the Triassic on the east of the East European Platform. These changes have been reflected in the geochemical features and magnetic properties of the rocks, the isotopic composition of chemical elements, the characteristics of the fauna, as well as the nature of the sediments. Permian sediments complete have an extremely complex geological structure, are characterized by a diversity of lithologic-facies composition and occurring of specific minerals, which are considered indicators of various types of lithogenesis (sulfate-carbonate rocks, coals, copper sandstones, schists, etc.). Based on lithological and paleomagnetic studies, paleogeographic reconstructions were performed. They showed that one of the factors of Perm sedimentation and related processes of the formation of ore and nonmetallic minerals are global climatic changes caused by Carboniferous-Permian glaciation.	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	Paleogeography	ru_RU
dc.subject	sedimentation the formation	ru_RU
dc.subject	mineral deposits	ru_RU
dc.subject	Permian	ru_RU
dc.subject	Triassic	ru_RU
dc.title	Paleogeographic causes of the formation of mineral deposits on the east of the East European platform in the Permian period	ru_RU
dc.type	Статьи в зарубежных журналах и сборниках	ru_RU