Prehistoric tsunamis and large earthquakes on the Kamchatskiy Peninsula, Kamchatka, based on tephrochronological data

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dc.contributor.author Melekestsev I.V.
dc.contributor.author Kurbatov A.V.
dc.contributor.author Pevzner M.M.
dc.contributor.author Sulerzhitskiy L.D.
dc.date.accessioned 2019-08-29T10:27:31Z
dc.date.available 2019-08-29T10:27:31Z
dc.date.issued 1995
dc.identifier http://repo.kscnet.ru/1110/
dc.identifier http://www.scopus.com/inward/record.url?eid=2-s2.0-0029501455&partnerID=40&md5=648bed1d597439047b233e36de5dc367
dc.identifier.citation Melekestsev I.V., Kurbatov A.V., Pevzner M.M., Sulerzhitskiy L.D. (1995) Prehistoric tsunamis and large earthquakes on the Kamchatskiy Peninsula, Kamchatka, based on tephrochronological data // Volcanology and Seismology. Vol. 16, No. 4-5. pp. 449-459.
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/4354
dc.description.abstract For the first time in Kamchatka, tephrochronology has been used to date paleoseismo-dislocations, tsunami deposits, and episodes of seismotectonic uplift that had occurred on the Kamchatskiy Peninsula for the past 2000 years. Four tephra markers have been used: three of the 1964, ~1260, and ~650 A.D. eruptions at Shiveluch Volcano and one of the ~250 A.D. caldera-forming eruption at Ksudach. The deposits of two 13th century and one 7th century tsunamis have been identified and dated. It has been found that Cape Kamchatskiy and Afrika were formed by two large seismotectonic landslides at the beginning of the Christian Era, simultaneously with an uplift of at least 35-40-km of the southeastern coast between the two capes.
dc.language.iso en
dc.subject 38.19.17 Землетрясения и сейсмотектоника
dc.title Prehistoric tsunamis and large earthquakes on the Kamchatskiy Peninsula, Kamchatka, based on tephrochronological data
dc.type Статья


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