GEOCHRONOLOGY OF BASALTS FROM THE VALLEY OF LAKES, MONGOLIA, AND THEIR CORRELATION WITH THE CENOZOIC SEDIMENTARY SEQUENCE

Show simple item record

dc.contributor.author Devyatkin E.V.
dc.contributor.author Balogh K.
dc.contributor.author Dudich A.
dc.date.accessioned 2021-06-24T08:05:43Z
dc.date.available 2021-06-24T08:05:43Z
dc.date.issued 2002
dc.identifier https://elibrary.ru/item.asp?id=21517828
dc.identifier.citation Russian Journal of Earth Sciences, 2002, 4, 5, 389-397
dc.identifier.issn 1681-1208
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/29270
dc.description.abstract The Valley of Lakes, Mongolia, is a key region in which to elaborate the geochronology of biostratigraphic horizons of the continental Paleogene and Neogene. Here, basaltic volcanism is developed widely. Basalt flow units are found alternating with and overlying sedimentary strata, while dikes and bosses cut through Paleocene, Oligocene, and Miocene faunal horizons. Analyzing biostratigraphic material in combination with K-Ar dating affords upgrading the biogeochronological subdivision and correlating some of the horizons with the mammalian zonation of Europe. The Valley of Lakes thus becomes the stratotype locality for Cenozoic continental sections in Inner Asia.
dc.subject CENOZOIC
dc.subject STRATIGRAPHY
dc.subject GEOCHRONOLOGY
dc.subject BASALTS
dc.subject RADIOMETRIC DATING
dc.subject FAUNA
dc.title GEOCHRONOLOGY OF BASALTS FROM THE VALLEY OF LAKES, MONGOLIA, AND THEIR CORRELATION WITH THE CENOZOIC SEDIMENTARY SEQUENCE
dc.type Статья
dc.subject.age Cenozoic
dc.subject.age Кайнозой ru


Files in this item

This item appears in the following Collection(s)

  • ELibrary
    Метаданные публикаций с сайта https://www.elibrary.ru

Show simple item record