KFU. Card publication. Comparative geochemistry of the basalts from Vesuvius and Batur volcanoes

KAZAN
FEDERAL UNIVERSITY

- RUS
- 中文
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COMPARATIVE GEOCHEMISTRY OF THE BASALTS FROM VESUVIUS AND BATUR VOLCANOES

Form of presentation

Conference proceedings in international journals and collections

Year of publication

2020

Язык

английский

Authors, employees of KFU

Kadyrov Rail Ilgizarovich, author

Bibliographic description in the original language

Kadyrov R., Minibaeva E. Comparative geochemistry of the basalts from Vesuvius and Batur volcanoes // IOP Conf. Ser. Earth Environ. Sci. 2020. Vol. 516, № 1. P. 012006.

Annotation

IOP Conference Series: Earth and Environmental Science

Keywords

Alkalinity, Basalt, Geochemistry, Mass spectrometry, Sedimentary rocks, Spectrum analysis, Volcanoes

The name of the journal

IOP Conference Series: Earth and Environmental Science

URL

https://www.scopus.com/record/display.uri?eid=2-s2.0-85087453921&origin=resultslist

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

https://repository.kpfu.ru/eng/?p_id=250626&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 geochemistry of the basalts from Vesuvius and Batur volcanoes // IOP Conf. Ser. Earth Environ. Sci. 2020. Vol. 516, № 1. P. 012006.	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/eng/?p_id=250626&p_lang=2	ru_RU
dc.description.abstract	IOP Conference Series: Earth and Environmental Science	ru_RU
dc.description.abstract	Sedimentary rocks can form both directly during eruptions and the destruction of effusive rocks. They can inherit the geochemical features of parent rocks. Therefore, the study of trace elements of the effusives is significant for the interpretation of the erosion source. This work provides information about trace element geochemistry of basalts from Vesuvius and Batur volcanoes, which are located at different ends of the Mediterranean-Alpine-Himalayan folded belt and represented by alkaline (subalkaline) type of magmas. The comparison of trace element concentration obtained by atomic emission spectral analysis and inductively coupled plasma mass spectrometry showed strong differences for a number of elements. Magma of Vesuvius, originating from a deep source, assimilated in its path the core material, which led to the eruption of lavas of the type EM I with high concentrations of Ba, Be, Cs, La, Rb, Mo, U, W, Zr. Batur relates to subduction arc volcanoes with the characteristic type of lavas HIMU, which are depleted of listed above chemical elements and enriched Bi. The basalts of these volcanoes have similar anomalies of the geochemical composition for most trace elements, suggesting that they have one close source that can be presented by subduction-modified oceanic lithosphere involved in generation of both HIMU and EM types.	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	Alkalinity	ru_RU
dc.subject	Basalt	ru_RU
dc.subject	Geochemistry	ru_RU
dc.subject	Mass spectrometry	ru_RU
dc.subject	Sedimentary rocks	ru_RU
dc.subject	Spectrum analysis	ru_RU
dc.subject	Volcanoes	ru_RU
dc.title	Comparative geochemistry of the basalts from Vesuvius and Batur volcanoes	ru_RU
dc.type	Conference proceedings in international journals and collections	ru_RU