КФУ. Карточка публикации. Comparative mineralogy and petrography of the basalts of Vesuvius and Batur volcanoes

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COMPARATIVE MINERALOGY AND PETROGRAPHY OF THE BASALTS OF VESUVIUS AND BATUR VOLCANOES

Форма представления

Тезисы и материалы конференций в зарубежных журналах и сборниках

Год публикации

2020

Язык

английский

Авторы, сотрудники КФУ

Кадыров Раиль Илгизарович, автор

Библиографическое описание на языке оригинала

Kadyrov R., Minibaeva E. Comparative mineralogy and petrography of the basalts of Vesuvius and Batur volcanoes // IOP Conf. Ser. Earth Environ. Sci. 2020. Vol. 516, № 1. P. 012007.

Аннотация

IOP Conference Series: Earth and Environmental Science

Ключевые слова

Aluminum, Basalt, Minerals, Viscosity, Volcanoes

Название журнала

IOP Conference Series: Earth and Environmental Science

URL

https://www.scopus.com/record/display.uri?eid=2-s2.0-85087461546&origin=resultslist

Пожалуйста, используйте этот идентификатор, чтобы цитировать или ссылаться на эту карточку

https://repository.kpfu.ru/?p_id=250624

Полная запись метаданных

Поле DC	Значение	Язык
dc.contributor.author	Кадыров Раиль Илгизарович	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	Kadyrov R., Minibaeva E. Comparative mineralogy and petrography of the basalts of Vesuvius and Batur volcanoes // IOP Conf. Ser. Earth Environ. Sci. 2020. Vol. 516, № 1. P. 012007.	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/?p_id=250624	ru_RU
dc.description.abstract	IOP Conference Series: Earth and Environmental Science	ru_RU
dc.description.abstract	In areas of active volcanic activity, sedimentary rocks can form both directly during eruptions and the destruction of effusive rocks. Therefore, the study of effusive parent rocks such as basalts is very important. This work provides information about the history of formation and geological structure of Vesuvius and Batur volcanoes, which are located at different ends of the Mediterranean-Alpine-Himalayan folded belt and have a similar layer-cone structure and they are represented by alkaline (subalkaline) type of magmas. Based on the research and literature data, it is found that modern basaltic samples from these volcanoes are mineralogically close. The basalt of Mount Batur was formed from lavas with higher aluminium content in the melt, higher viscosity, with strong degassing and rapid cooling. The formation of effusive rocks of Vesuvius, on the contrary, is associated with a lower viscosity of lava, a lower content of aluminium and its slower cooling. They underwent more significant secondary changes.	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	Aluminum	ru_RU
dc.subject	Basalt	ru_RU
dc.subject	Minerals	ru_RU
dc.subject	Viscosity	ru_RU
dc.subject	Volcanoes	ru_RU
dc.title	Comparative mineralogy and petrography of the basalts of Vesuvius and Batur volcanoes	ru_RU
dc.type	Тезисы и материалы конференций в зарубежных журналах и сборниках	ru_RU