Carbonate sequences of the Middle Ordovician-Silurian of the Pechora-Barents Sea megabasin
Authors:
About authors
- All-Russian Research Institute of Geology and Mineral Resources of the World Ocean
Abstract
Application of the sequence-stratigraphy method has allowed to trace the principal stages in development of the Middle Ordovician – Silurian sedimentation within the Pechora-Barents sedimentary megabasin. There were established, on this base, some regularities in distribution of reservoirs and seals in the geologic section of the Low-Middle Paleozoic.
Область исследования:
(Archived) Problems of shelf development: geology and ocean engineering
Funding:
None
Similar articles
Development of geoelectrochemical technologies and their complex use in hydrocarbon prospecting
2008 M. B. Shtokalenko, S. G. Alekseev, S. A. Veshev, N. A. Voroshilov, O. F. Putikov
Modern sediments of the eastern part of the Arctic Ocean and their geologic significance
2008 V. Ya. Kabankov, I. A. Andreeva
Methodological principles of landscape-geoecological studies of the shelf on the example of the Barents Sea
2008 I. A. Andreeva, A. G. Zinchenko, B. G. Vanshtein, O. A. Kiiko, V. I. Petrova
Influence of complex hydrology on vertical props of submersible and semi-submersible drilling rigs
2008 V. V. Vasileva, T. D. Mordvina