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14C Ages of Tephra Layers from the Holocene Deposits of Kunashir Island (Russian Far East)

dc.contributor.authorRazjigaeva, N. G.
dc.contributor.authorGrebennikova, T. A.
dc.contributor.authorGanzey, L. A.
dc.contributor.authorBazarova, V. B.
dc.contributor.authorMokhova, L. M.
dc.contributor.authorKorotky, A. M.
dc.contributor.authorSulerzhitsky, L. D.
dc.date.accessioned2021-02-11T21:31:41Z
dc.date.available2021-02-11T21:31:41Z
dc.date.issued1998-01-01
dc.identifier.citationRazjigaeva, N. G., Grebennikova, T. A., Ganzey, L. A., Bazarova, V. B., Mokhova, L. M., Korotky, A. M., & Sulerzhitsky, L. D. (1998). 14C ages of tephra layers from the Holocene deposits of Kunashir Island (Russian Far East). Radiocarbon, 40(2), 841-847.
dc.identifier.issn0033-8222
dc.identifier.doi10.1017/S0033822200018804
dc.identifier.urihttp://hdl.handle.net/10150/654391
dc.descriptionFrom the 16th International Radiocarbon Conference held in Gronigen, Netherlands, June 16-20, 1997.
dc.description.abstractHolocene deposits from the central and southern regions of the Kunashir Island contain tephra from 12 volcanic eruptions (Kn1-12). We studied radiocarbon data, mineralogical composition, and distribution of the tephra layers in different Holocene facies. The main sources of the Holocene tephra samples were the volcanoes of Hokkaido Island. The distribution of ash layers on Kunashir Island allows us to estimate their direction. Ash layers can be reliable markers for age determination of different coastal landforms on open oceanic shores. We propose here a tephrastratigraphical scheme for different Middle-Late Holocene facies.
dc.language.isoen
dc.publisherDepartment of Geosciences, The University of Arizona
dc.relation.urlhttp://radiocarbon.webhost.uits.arizona.edu/
dc.rightsCopyright © by the Arizona Board of Regents on behalf of the University of Arizona. All rights reserved.
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/
dc.subjectHolocene
dc.subjectupper Holocene
dc.subjectmicrofossils
dc.subjectmiospores
dc.subjectpalynomorphs
dc.subjectpollen
dc.subjectFar East
dc.subjectJapan
dc.subjectvolcanoes
dc.subjectbiostratigraphy
dc.subjectPlantae
dc.subjectstratigraphy
dc.subjecteruptions
dc.subjectcorrelation
dc.subjectalgae
dc.subjectmineral composition
dc.subjectigneous rocks
dc.subjectpyroclastics
dc.subjectvolcanic ash
dc.subjectvolcanic rocks
dc.subjectmiddle Holocene
dc.subjectHokkaido
dc.subjectvolcanism
dc.subjectKunashir Island
dc.subjectKuril Islands
dc.subjectRussian Far East
dc.subjectRussian Pacific region
dc.subjectSakhalin Russian Federation
dc.subjectdistribution
dc.subjectdiatoms
dc.subjectRussian Federation
dc.subjectCommonwealth of Independent States
dc.subjectAsia
dc.subjectCenozoic
dc.subjectQuaternary
dc.subjectC 14
dc.subjectcarbon
dc.subjectdates
dc.subjectisotopes
dc.subjectradioactive isotopes
dc.subjectabsolute age
dc.title14C Ages of Tephra Layers from the Holocene Deposits of Kunashir Island (Russian Far East)
dc.typeProceedings
dc.typetext
dc.identifier.journalRadiocarbon
dc.description.noteThis material was digitized as part of a cooperative project between Radiocarbon and the University of Arizona Libraries.
dc.description.collectioninformationThe Radiocarbon archives are made available by Radiocarbon and the University of Arizona Libraries. Contact lbry-journals@email.arizona.edu for further information.
dc.eprint.versionFinal published version
dc.description.admin-noteMigrated from OJS platform February 2021
dc.source.volume40
dc.source.issue2
dc.source.beginpage841
dc.source.endpage847
refterms.dateFOA2021-02-11T21:31:41Z


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