Яндекс.Метрика

N.V. Sennikov, R.A. Khabibulina, O.T. Obut, N.V. Novozhilova, D.A. Tokarev, V.A. Luchinina

Issue: 4 , Volume: 60 , Уear of publication: 2019
Serial edition: Russian Geology and Geophysics
Pages: 451-471

Abstract

This paper discusses the structure and facies variability of the Silurian mixed terrigenous-carbonate strata and presents new paleontological and biostratigraphic data. It attempts to refine the stratigraphic position and provide new lithologic evidence (markers) for regional manifestations of global sedimentary events (Mulde transgressive-regressive and Linde regressive events) in the Altai sections. The chronostratigraphic position of the Kuimov Horizon, a regional stratigraphic unit, has been defined based on graptolite and conodont faunas.
индекс в базе ИАЦ: 046109