KFU. Card publication. Comparative mineralogy and petrography of the basalts of Vesuvius and Batur volcanoes

KAZAN
FEDERAL UNIVERSITY

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

Form of presentation

Conference proceedings in international journals and collections

Year of publication

2020

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Authors, employees of KFU

Kadyrov Rail Ilgizarovich, author

Bibliographic description in the original language

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.

Annotation

IOP Conference Series: Earth and Environmental Science

Keywords

Aluminum, Basalt, Minerals, Viscosity, Volcanoes

The name of the journal

IOP Conference Series: Earth and Environmental Science

URL

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

Please use this ID to quote from or refer to the card

https://repository.kpfu.ru/eng/?p_id=250624&p_lang=2

Full metadata record

Field DC	Value	Language
dc.contributor.author	Kadyrov Rail Ilgizarovich	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/eng/?p_id=250624&p_lang=2	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	Conference proceedings in international journals and collections	ru_RU