Please use this identifier to cite or link to this item: http://elar.urfu.ru/handle/10995/101722
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dc.contributor.authorPetrova, E. V.en
dc.contributor.authorGrokhovsky, V. I.en
dc.contributor.authorKohout, T.en
dc.contributor.authorMuftakhetdinova, R. F.en
dc.contributor.authorYakovlev, G. A.en
dc.date.accessioned2021-08-31T14:59:22Z-
dc.date.available2021-08-31T14:59:22Z-
dc.date.issued2019-
dc.identifier.citationShock-Wave Experiment with the Chelyabinsk LL5 Meteorite: Experimental Parameters and the Texture of the Shock-Affected Material / E. V. Petrova, V. I. Grokhovsky, T. Kohout, et al. — DOI 10.1134/S0016702919080081 // Geochemistry International. — 2019. — Vol. 57. — Iss. 8. — P. 923-930.en
dc.identifier.issn167029-
dc.identifier.otherFinal2
dc.identifier.otherAll Open Access, Green3
dc.identifier.otherhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85070231690&doi=10.1134%2fS0016702919080081&partnerID=40&md5=2f65ac0f898f80f569963cb1d7b1079f
dc.identifier.otherhttps://helda.helsinki.fi/bitstream/10138/319076/1/Petrova_et_al_Chelyabinsk_spherical_shock_GI_2019._author_version.pdfm
dc.identifier.urihttp://elar.urfu.ru/handle/10995/101722-
dc.description.abstractAbstract: A spherical geometry shock experiment with the light-colored lithology material of the Chelyabinsk LL5 ordinary chondrite was carried out. The material was affected by shock and thermal metamorphism whose grade ranged from initial stage S3-4 to complete melting. The temperature and pressure were estimated at >2000°С and >90 GPa. The textural shock effects were studied by optical and electron microscopy. A single experimental impact has produced the whole the range of shock pressures and temperatures and, correspondingly, four zones identified by petrographic analysis: (1) a melt zone, (2) a zone of melting silicates, (3) a black ring zone, and (4) a zone of weakly shocked initial material. The following textural features of the material were identified: displacement of the metal and troilite phases from the central melt zone; the development of a zone of mixed lithology (light-colored fragments in silicate melt); the origin of a dark-colored lithology ring; and the generation of radiating shock veinlets. The experimental sample shows four textural zones that correspond to the different lithology types of the Chelyabinsk LL5 meteorite found in fragments of the meteoritic shower in the collection at the Ural Federal University. Our results prove that shock wave loading experiment can be successfully applied in modeling of space shocks and can be used to experimentally model processes at the small bodies of the solar system. © 2019, Pleiades Publishing, Ltd.en
dc.format.mimetypeapplication/pdfen
dc.language.isoenen
dc.publisherPleiades Publishingen
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.sourceGeochem. Int.2
dc.sourceGeochemistry Internationalen
dc.subjectCHELYABINSK METEORITEen
dc.subjectORDINARY CHONDRITEen
dc.subjectSHOCK EXPERIMENTen
dc.subjectSHOCK METAMORPHISMen
dc.subjectSPHERICAL SHOCKen
dc.subjectSTRUCTUREen
dc.subjectTEXTUREen
dc.subjectLITHOLOGYen
dc.subjectMELTINGen
dc.subjectSHOCK WAVESen
dc.subjectSILICATESen
dc.subjectSTRUCTURE (COMPOSITION)en
dc.subjectTEXTURESen
dc.subjectEXPERIMENTAL PARAMETERSen
dc.subjectOPTICAL AND ELECTRON MICROSCOPIESen
dc.subjectORDINARY CHONDRITESen
dc.subjectPETROGRAPHIC ANALYSISen
dc.subjectSHOCK METAMORPHISMen
dc.subjectSPHERICAL GEOMETRIESen
dc.subjectSPHERICAL SHOCKSen
dc.subjectTEMPERATURE AND PRESSURESen
dc.subjectMETEORITESen
dc.subjectEXPERIMENTen
dc.subjectMELTINGen
dc.subjectORDINARY CHONDRITEen
dc.subjectSHOCK METAMORPHISMen
dc.subjectSHOCK WAVEen
dc.subjectTEXTUREen
dc.subjectCHELYABINSK [RUSSIAN FEDERATION]en
dc.subjectRUSSIAN FEDERATIONen
dc.titleShock-Wave Experiment with the Chelyabinsk LL5 Meteorite: Experimental Parameters and the Texture of the Shock-Affected Materialen
dc.typeArticleen
dc.typeinfo:eu-repo/semantics/articleen
dc.typeinfo:eu-repo/semantics/publishedVersionen
dc.identifier.rsi41625177-
dc.identifier.doi10.1134/S0016702919080081-
dc.identifier.scopus85070231690-
local.contributor.employeePetrova, E.V., Ural Federal University, Institute of Physics and Technology, Yekaterinburg, 620002, Russian Federation
local.contributor.employeeGrokhovsky, V.I., Ural Federal University, Institute of Physics and Technology, Yekaterinburg, 620002, Russian Federation
local.contributor.employeeKohout, T., University of Helsinki, Faculty of Science, Helsinki, PL64, Finland
local.contributor.employeeMuftakhetdinova, R.F., Ural Federal University, Institute of Physics and Technology, Yekaterinburg, 620002, Russian Federation
local.contributor.employeeYakovlev, G.A., Ural Federal University, Institute of Physics and Technology, Yekaterinburg, 620002, Russian Federation
local.description.firstpage923-
local.description.lastpage930-
local.issue8-
local.volume57-
dc.identifier.wos000479059100009-
local.contributor.departmentUral Federal University, Institute of Physics and Technology, Yekaterinburg, 620002, Russian Federation
local.contributor.departmentUniversity of Helsinki, Faculty of Science, Helsinki, PL64, Finland
local.identifier.pure24b4857b-2bc8-4613-be8f-57064c1c5fd6uuid
local.identifier.pure10467703-
local.identifier.eid2-s2.0-85070231690-
local.identifier.wosWOS:000479059100009-
Appears in Collections:Научные публикации ученых УрФУ, проиндексированные в SCOPUS и WoS CC

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