Lithological and seismic-stratigraphic characteristics of the Barents Sea shelf section according to the geological-geophysical research data
UDC: 553.98(571.1)(–17)+550.3
DOI: -
Authors:
BORODKIN VLADIMIR N.
1,2,
SMIRNOV OLEG A.1,3,
LUKASHOV ANDREY V.3,
SAMITOVA VENERA I.1
1 A. Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of Russian Academy of Sciences, Tyumen, Russia
2 Tyumen Industrial University, Tyumen, Russia
3 INGEOSERVICE LLC, Tyumen, Russia
Keywords: the Barents Sea shelf, seismic complex, reflecting horizon, formation speed, clinoform reflections
Annotation:
The authors of the article, based on the seismic data, core material from drilled wells and descriptions of outcrops on the islands and archipelagos, present lithological-seismic-stratigraphic characteristics of the Archean-Lower Proterozoic, Upper Proterozoic, Ordovician-Middle Devonian, Upper Devonian-Lower Permian, Lower-Upper Permian, Triassic, Lower-Middle Jurassic, Upper Jurassic and Cretaceous seismic-stratigraphic complexes.
The lithological composition and textural features of each complex rocks is briefly described, the reflecting seismic horizons are identified in the section and their morphological characteristics are given. For the Triassic and Jurassic complexes, some differences in the indexing of reflective seismic horizons by different researchers have been shown.
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