Churikova, Tatiana G.

[["dc.bibliographiccitation.firstpage","659"],["dc.bibliographiccitation.issue","5"],["dc.bibliographiccitation.journal","Contributions to Mineralogy and Petrology"],["dc.bibliographiccitation.lastpage","687"],["dc.bibliographiccitation.volume","159"],["dc.contributor.author","Volynets, Anna O."],["dc.contributor.author","Churikova, Tatiana G."],["dc.contributor.author","Woerner, Gerhard"],["dc.contributor.author","Gordeychik, Boris N."],["dc.contributor.author","Layer, Paul"],["dc.date.accessioned","2018-11-07T08:43:29Z"],["dc.date.available","2018-11-07T08:43:29Z"],["dc.date.issued","2010"],["dc.description.abstract","New (40)Ar/(39)Ar and published (14)C ages constrain voluminous mafic volcanism of the Kamchatka back-arc to Miocene (3-6 Ma) and Late Pleistocene to Holocene (< 1 Ma) times. Trace elements and isotopic compositions show that older rocks derived from a depleted mantle through subduction fluid-flux melting (> 20%). Younger rocks form in a back arc by lower melting degrees involving enriched mantle components. The arc front and Central Kamchatka Depression are also underlain by plateau lavas and shield volcanoes of Late Pleistocene age. The focus of these voluminous eruptions thus migrated in time and may be the result of a high fluid flux in a setting where the Emperor seamount subducts and the slab steepens during rollback during terrain accretions. The northern termination of Holocene volcanism locates the edge of the subducting Pacific plate below Kamchatka, a \"slab-edge-effect\" is not observed in the back arc region."],["dc.identifier.doi","10.1007/s00410-009-0447-9"],["dc.identifier.isi","000276276300004"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?goescholar/4176"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/19974"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Springer"],["dc.relation.issn","0010-7999"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.title","Mafic Late Miocene-Quaternary volcanic rocks in the Kamchatka back arc region: implications for subduction geometry and slab history at the Pacific-Aleutian junction"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.issue","13"],["dc.bibliographiccitation.journal","Geochimica et Cosmochimica Acta"],["dc.bibliographiccitation.volume","73"],["dc.contributor.author","Volynets, Anna O."],["dc.contributor.author","Churikova, Tatiana G."],["dc.contributor.author","Woerner, Gerhard"],["dc.date.accessioned","2018-11-07T08:29:17Z"],["dc.date.available","2018-11-07T08:29:17Z"],["dc.date.issued","2009"],["dc.format.extent","A1393"],["dc.identifier.isi","000267229903474"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/16610"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Pergamon-elsevier Science Ltd"],["dc.publisher.place","Oxford"],["dc.relation.conference","19th Annual VM Goldschmidt Conference"],["dc.relation.eventlocation","Davos, SWITZERLAND"],["dc.relation.issn","0016-7037"],["dc.title","Mantle sources and fluids in the Northern Kamchatka back arc"],["dc.type","conference_abstract"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","212"],["dc.bibliographiccitation.journal","Lithos"],["dc.bibliographiccitation.lastpage","224"],["dc.bibliographiccitation.volume","322"],["dc.contributor.author","Nekrylov, Nikolai"],["dc.contributor.author","Portnyagin, Maxim V."],["dc.contributor.author","Kamenetsky, Vadim S."],["dc.contributor.author","Mironov, Nikita L."],["dc.contributor.author","Churikova, Tatiana G."],["dc.contributor.author","Plechov, Pavel Yu."],["dc.contributor.author","Abersteiner, Adam"],["dc.contributor.author","Gorbach, Natalia V."],["dc.contributor.author","Gordeychik, Boris N."],["dc.contributor.author","Krasheninnikov, Stepan P."],["dc.contributor.author","Tobelko, Daria P."],["dc.contributor.author","Shur, Maria Yu."],["dc.contributor.author","Tetroeva, Sofia A."],["dc.contributor.author","Volynets, Anna O."],["dc.contributor.author","Hoernle, Kaj"],["dc.contributor.author","Wörner, Gerhard"],["dc.date.accessioned","2020-12-10T15:20:17Z"],["dc.date.available","2020-12-10T15:20:17Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.1016/j.lithos.2018.10.011"],["dc.identifier.issn","0024-4937"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/72608"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Chromium spinel in Late Quaternary volcanic rocks from Kamchatka: Implications for spatial compositional variability of subarc mantle and its oxidation state"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]