AGE OF ROCKS IN THE BAIKAL-MUYA FOLDBELT

dc.contributor.authorRytsk E.Yu.
dc.contributor.authorRizvanova N.G.
dc.contributor.authorKrimsky R.Sh.
dc.contributor.authorShalaev V.S.
dc.contributor.authorAmelin Yu.V.
dc.contributor.authorMitrofanov G.L.
dc.contributor.authorMitrofanova N.N.
dc.contributor.authorPerelyaev V.I.
dc.date.accessioned2021-02-22T07:40:49Z
dc.date.available2021-02-22T07:40:49Z
dc.date.issued2001
dc.description.abstractThe presented results of U-Pb zircon dating (those for individual grains included) and Sm-Nd isochron ages for whole-rock samples and mineral fraction characterize magmatic complexes of the Muya segment of the Baikal-Muya foldbelt. New isotopic dates indicate the Late Riphean-Vendian age of volcanogenic-sedimentary and igneous rocks, which have been formed in the Muya segment during the Early Baikalian (from about 1.0 to 0.8 Ga) and Late Baikalian (0.8-0.62 Ga) stages of tectogenesis. The distinguished syntectonic granitoids of the Early Baikalian stage mark a collision event that happened 0.8 Ga ago. The results obtained are used to refine the traditional scheme of Precambrian stratigraphy and magmatism in the Middle Vitim Mountains.
dc.identifierhttps://elibrary.ru/item.asp?id=13377000
dc.identifier.citationStratigraphy and Geological Correlation, 2001, 9, 4, 315-326
dc.identifier.issn0869-5938
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/25325
dc.subjectPrecambrian
dc.subjectRiphean
dc.subjectVendian
dc.subjectBaikal-Muya foldbelt
dc.subject.agePrecambrian::Proterozoic::Neoproterozoic::Vendianen
dc.titleAGE OF ROCKS IN THE BAIKAL-MUYA FOLDBELT
dc.typeСтатья

Файлы

Коллекции