Carbonate sequences of the Middle Ordovician-Silurian of the Pechora-Barents Sea megabasin
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- 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
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