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
Similar articles
Estimation of complexity of engineering-geological conditions on the experience of Far East region
2008 S. V. Kvashuk, E. V. Fedorenko