Small Shelly Fossils in the Cambrian Basement of the West Siberian Geosyneclise
- Authors: Novozhilova N.V.1,2, Korovnikov I.V.1,2
-
Affiliations:
- Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences
- Novosibirsk National Research State University
- Issue: Vol 27, No 1 (2019)
- Pages: 1-8
- Section: Article
- URL: https://ogarev-online.ru/0869-5938/article/view/178013
- DOI: https://doi.org/10.1134/S0869593819010040
- ID: 178013
Cite item
Abstract
This paper describes for the first time the entire Cambrian skeletal problematics from the parametric well Vostok-1 (Tomsk oblast, eastern part of the West Siberian Plate) found in the Lower Cambrian Churbiga Formation, Middle Cambrian Pudzhelga Formation, and Upper Cambrian Kondes and Shedelga formations. The investigation has made it possible to detail the biostratigraphic division of the Lower Cambrian in the studied well using the small shelly fossils and to reveal confinement of the main findings of problematic skeletal remains to the shallow carbonate shelf settings.
About the authors
N. V. Novozhilova
Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences; Novosibirsk National Research State University
Author for correspondence.
Email: NovozhilovaNV@ipgg.sbras.ru
Russian Federation, Novosibirsk, 630090; Novosibirsk, 630090
I. V. Korovnikov
Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences; Novosibirsk National Research State University
Email: NovozhilovaNV@ipgg.sbras.ru
Russian Federation, Novosibirsk, 630090; Novosibirsk, 630090
Supplementary files
