THE OKHOTSK-CHUKOTKA VOLCANIC BELT: AGE OF ITS NORTHERN PART ACCORDING TO NEW AR-AR AND U-PB GEOCHRONOLOGICAL DATA

dc.contributor.authorTikhomirov P.L.
dc.contributor.authorAkinin V.V.
dc.contributor.authorIspolatov V.O.
dc.contributor.authorAlexander P.
dc.contributor.authorCherepanova I.Yu.
dc.contributor.authorZagoskin V.V.
dc.date.accessioned2024-07-20T12:13:53Z
dc.date.available2024-07-20T12:13:53Z
dc.date.issued2006
dc.description.abstractCurrent geochronological data on the Okhotsk-Chukotka volcanic belt (OCVB) and relevant problems are discussed. The belt evolution is suggested to be modeled based on 40Ar/39Ar and U-Pb dates more useful in several aspects than common K-Ar or Rb-Sr dates and methods of paleobotanical correlation. Based on new 40Ar/39Ar and U-Pb dates obtained for volcanic rocks in the OCVB northern part, the younger (Coniacian) age is established for lower stratigraphic units in the Central Chukotka segment of the belt, and the eastward migration of volcanic activity is shown for terminal stages of this structure evolution. ©MAIK 'Nauka/ Interperiodica' 2006.
dc.identifierhttps://elibrary.ru/item.asp?id=13519575
dc.identifier.citationStratigraphy and Geological Correlation, 2006, 14, 5, 524-537
dc.identifier.doi10.1134/S0869593806050054
dc.identifier.issn0869-5938
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/44460
dc.subjectACTIVE CONTINENTAL MARGINS
dc.subjectGEOCHRONOLOGY
dc.subjectOKHOTSK-CHUKOTKA BELT
dc.subjectSTRATIGRAPHY
dc.subjectVOLCANISM
dc.subject.ageМезозой::Меловая::Верхний::Коньякский
dc.subject.ageMesozoic::Cretaceous::Upper::Coniacian
dc.titleTHE OKHOTSK-CHUKOTKA VOLCANIC BELT: AGE OF ITS NORTHERN PART ACCORDING TO NEW AR-AR AND U-PB GEOCHRONOLOGICAL DATA
dc.typeСтатья

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