Evidence for compressionally induced high subsidence rates in the Kurile Basin (Okhotsk Sea)

dc.contributor.authorBaranov B.V.
dc.contributor.authorWerner Reinhard
dc.contributor.authorHoernle K.A.
dc.contributor.authorTsoy I.B.
dc.contributor.authorvan den Bogaard Paul
dc.contributor.authorTararin I.A.
dc.date.accessioned2019-08-30T08:18:04Z
dc.date.available2019-08-30T08:18:04Z
dc.date.issued2002
dc.identifierhttp://repo.kscnet.ru/2167/
dc.identifierhttp://dx.doi.org/10.1016/S0040-1951(02)00081-1
dc.identifier.citationBaranov B.V., Werner Reinhard, Hoernle K.A., Tsoy I.B., van den Bogaard Paul, Tararin I.A. (2002) Evidence for compressionally induced high subsidence rates in the Kurile Basin (Okhotsk Sea) // Tectonophysics. Vol. 350, No. 1. pp. 63-97. doi: 10.1016/S0040-1951(02)00081-1.
dc.identifier.doi10.1016/S0040-1951(02)00081-1
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/5232
dc.language.isoen
dc.subject38.37.27 Петрография океанических пород и подводный вулканизм
dc.subjectГригорьева
dc.titleEvidence for compressionally induced high subsidence rates in the Kurile Basin (Okhotsk Sea)
dc.typeСтатья

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