KFU. Card publication. SPACE IRON OXIDE MICROSPHERES: ORIGIN AND TYPOMORPHIC FEATURES

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FEDERAL UNIVERSITY

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SPACE IRON OXIDE MICROSPHERES: ORIGIN AND TYPOMORPHIC FEATURES

Form of presentation

Conference proceedings in Russian journals and collections

Year of publication

2019

Язык

английский

Authors, employees of KFU

Bakhtin Anatoliy Iosifovich, author

Gusev Aleksandr Vasilevich, author

Sungatullin Rafael Kharisovich, author

Other authors

Celmovich Vladimir Anatolevich, author

Bibliographic description in the original language

Gusev A. V., Bakhtin A. I., Sungatullin R. Kh., Tselmovich V. A. SPACE IRON OXIDE MICROSPHERES: ORIGIN AND TYPOMORPHIC FEATURES // THE TENTH MOSCOW SOLAR SYSTEM SYMPOSIUM, Moscow, IKI RAS, 7-11 October 2019. Moscow, 2019. P. 447-449.

Annotation

THE TENTH MOSCOW SOLAR SYSTEM SYMPOSIUM

Keywords

meteoroids,Earth?s atmosphere, iron oxide microspheres, typomorphic features, cosmic origin

The name of the journal

THE TENTH MOSCOW SOLAR SYSTEM SYMPOSIUM

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

https://repository.kpfu.ru/eng/?p_id=212398&p_lang=2

Full metadata record

Field DC	Value	Language
dc.contributor.author	Bakhtin Anatoliy Iosifovich	ru_RU
dc.contributor.author	Gusev Aleksandr Vasilevich	ru_RU
dc.contributor.author	Sungatullin Rafael Kharisovich	ru_RU
dc.contributor.author	Celmovich Vladimir Anatolevich	ru_RU
dc.date.accessioned	2019-01-01T00:00:00Z	ru_RU
dc.date.available	2019-01-01T00:00:00Z	ru_RU
dc.date.issued	2019	ru_RU
dc.identifier.citation	Gusev A. V., Bakhtin A. I., Sungatullin R. Kh., Tselmovich V. A. SPACE IRON OXIDE MICROSPHERES: ORIGIN AND TYPOMORPHIC FEATURES // THE TENTH MOSCOW SOLAR SYSTEM SYMPOSIUM, Moscow, IKI RAS, 7-11 October 2019. Moscow, 2019. P. 447-449.	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/eng/?p_id=212398&p_lang=2	ru_RU
dc.description.abstract	THE TENTH MOSCOW SOLAR SYSTEM SYMPOSIUM	ru_RU
dc.description.abstract	In the sedimentary rocks of the Earth, metal spherical particles (microsphere} are often found, ranging in size from the first to several hundred micrometers across. They are composed of native iron, wustite, magnetite, have magnetism and therefore are relatively easy to extract from finely dispersed terrigenous and carbonate rocks. It is believed that the majority of metallic microspheres are of cosmic origin and are ubiquitous in the rocks of the Earth, mainly in the form of iron oxide (magnetite) microspheres. This implies the possibility of using such objects for the purposes of global stratigraphic correlation of sedimentary strata. To date, the typomorphic features of iron oxide microspheres remain underexplored. In this paper, we attempted to identify the typomorphic features of cosmic iron oxide microspheres, depending on the conditions of their formation.	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	meteoroids	ru_RU
dc.subject	Earth?s atmosphere	ru_RU
dc.subject	iron oxide microspheres	ru_RU
dc.subject	typomorphic features	ru_RU
dc.subject	cosmic origin	ru_RU
dc.title	SPACE IRON OXIDE MICROSPHERES: ORIGIN AND TYPOMORPHIC FEATURES	ru_RU
dc.type	Conference proceedings in Russian journals and collections	ru_RU