Sammendrag
A total of eleven Middle - Upper Carboniferous and twelve Lower Permian
conodont assemblage zones and subzones from 21 sampled sections in
Novaya Zemlya and from three wells in the Pechora Sea Shelf are defined
in this study. On Novaya Zemlya conodont samples were collected
systematically from four regions that represent a wide transition from
(near-shore) shallow to deep depositional environments/settings.
Approximately 160 samples contained conodonts. 104 conodont taxa are
recognized. Analysis of the distribution of these conodont taxa has
resulted in the recognition of 23 local conodont zones and subzones,
most of which are assemblage zones. Chronostratigraphic correlation
indicates that these zones range from Early Bashkirian
(Declinognathodus noduliferus Assemblage Zone) to Late Artinskian
(Neostreptognathodus pequopensis Assemblage Zone). In the Carboniferous
part of the succession, conodont zones are defined from both shallow
and basinal facies. Early Permian conodont assemblages obtained from
basinal facies are essentially different from coeval assemblages from
shallow water deposits. The conodont assemblages of Novaya Zemlya are
compared with zonal assemblages from type sections of the Russian
Platform and the Urals, which has provided a precise dating of local
stratigraphic units. In addition, correlation of the Middle
Carboniferous-Lower Permian sections of Novaya Zemlya with those of the
Sverdrup Basin (Arctic Canada) and Svalbard is possible based on the
defined conodont zones. Conodont Colour Alteration Index (CAI) isopach
maps have been prepared for the Middle Carboniferous and Upper
Carboni-ferous - Lower Permian from Novaya Zemlya and Pechora Sea
Shelf. An analysis of these maps allows identification of potentially
oil-producing deposits of Middle Carboniferous - Lower Permian of the
Pechora Shelf; potential gas-producing deposits of this age may occur
in the southern and northern areas of Novaya Zemlya. Additionally,
because of the regular distribution in the CAI values, oil- and
gas-producing rocks may be present to the west and north of Novaya
Zemlya.
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