- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
-
Arctic Ocean
-
Barents Sea (1)
-
Kara Sea (6)
-
-
Arctic region
-
Russian Arctic
-
Novaya Zemlya (2)
-
-
-
Asia
-
Krasnoyarsk Russian Federation
-
Taymyr Dolgan-Nenets Russian Federation
-
Taymyr Peninsula (1)
-
-
-
Siberia (1)
-
Tyumen Russian Federation
-
Yamal-Nenets Russian Federation
-
Yamal (9)
-
-
-
West Siberia
-
Siberian Lowland (2)
-
-
Yakutia Russian Federation (1)
-
-
Commonwealth of Independent States
-
Russian Federation
-
Arkhangelsk Russian Federation
-
Novaya Zemlya (2)
-
-
Krasnoyarsk Russian Federation
-
Taymyr Dolgan-Nenets Russian Federation
-
Taymyr Peninsula (1)
-
-
-
Polar Urals
-
Pai-Khoi (1)
-
-
Russian Arctic
-
Novaya Zemlya (2)
-
-
Tyumen Russian Federation
-
Yamal-Nenets Russian Federation
-
Yamal (9)
-
-
-
Yakutia Russian Federation (1)
-
-
Urals
-
Novaya Zemlya (2)
-
Polar Urals
-
Pai-Khoi (1)
-
-
-
West Siberia
-
Siberian Lowland (2)
-
-
-
Eurasia (1)
-
Europe
-
Arkhangelsk Russian Federation
-
Novaya Zemlya (2)
-
-
-
-
commodities
-
energy sources (1)
-
oil and gas fields (4)
-
petroleum
-
natural gas (2)
-
-
-
elements, isotopes
-
carbon
-
C-14 (1)
-
-
isotopes
-
radioactive isotopes
-
C-14 (1)
-
-
-
-
fossils
-
Chordata
-
Vertebrata
-
Tetrapoda
-
Mammalia
-
Theria
-
Eutheria
-
Proboscidea
-
Elephantoidea
-
Elephantidae
-
Mammuthus
-
Mammuthus primigenius (1)
-
-
-
-
-
-
-
-
-
-
-
-
geologic age
-
Cenozoic
-
Quaternary
-
Pleistocene
-
upper Pleistocene (1)
-
-
upper Quaternary (1)
-
-
-
Mesozoic
-
Cretaceous
-
Lower Cretaceous
-
Aptian
-
lower Aptian (1)
-
-
Berriasian (2)
-
Neocomian (2)
-
-
Upper Cretaceous
-
Cenomanian (1)
-
-
-
Jurassic
-
Bazhenov Formation (1)
-
-
Triassic (1)
-
-
Paleozoic
-
Carboniferous (1)
-
Devonian (1)
-
Permian (1)
-
upper Paleozoic (1)
-
-
-
Primary terms
-
absolute age (1)
-
Arctic Ocean
-
Barents Sea (1)
-
Kara Sea (6)
-
-
Arctic region
-
Russian Arctic
-
Novaya Zemlya (2)
-
-
-
Asia
-
Krasnoyarsk Russian Federation
-
Taymyr Dolgan-Nenets Russian Federation
-
Taymyr Peninsula (1)
-
-
-
Siberia (1)
-
Tyumen Russian Federation
-
Yamal-Nenets Russian Federation
-
Yamal (9)
-
-
-
West Siberia
-
Siberian Lowland (2)
-
-
Yakutia Russian Federation (1)
-
-
carbon
-
C-14 (1)
-
-
Cenozoic
-
Quaternary
-
Pleistocene
-
upper Pleistocene (1)
-
-
upper Quaternary (1)
-
-
-
Chordata
-
Vertebrata
-
Tetrapoda
-
Mammalia
-
Theria
-
Eutheria
-
Proboscidea
-
Elephantoidea
-
Elephantidae
-
Mammuthus
-
Mammuthus primigenius (1)
-
-
-
-
-
-
-
-
-
-
-
continental shelf (3)
-
energy sources (1)
-
Eurasia (1)
-
Europe
-
Arkhangelsk Russian Federation
-
Novaya Zemlya (2)
-
-
-
faults (1)
-
geophysical methods (3)
-
glacial geology (1)
-
isotopes
-
radioactive isotopes
-
C-14 (1)
-
-
-
Mesozoic
-
Cretaceous
-
Lower Cretaceous
-
Aptian
-
lower Aptian (1)
-
-
Berriasian (2)
-
Neocomian (2)
-
-
Upper Cretaceous
-
Cenomanian (1)
-
-
-
Jurassic
-
Bazhenov Formation (1)
-
-
Triassic (1)
-
-
oil and gas fields (4)
-
orogeny (1)
-
paleogeography (1)
-
Paleozoic
-
Carboniferous (1)
-
Devonian (1)
-
Permian (1)
-
upper Paleozoic (1)
-
-
petroleum
-
natural gas (2)
-
-
plate tectonics (1)
-
sedimentary rocks
-
clastic rocks (1)
-
-
sedimentation (1)
-
sediments
-
clastic sediments
-
diamicton (1)
-
-
peat (1)
-
-
tectonics (3)
-
-
sedimentary rocks
-
sedimentary rocks
-
clastic rocks (1)
-
-
-
sediments
-
sediments
-
clastic sediments
-
diamicton (1)
-
-
peat (1)
-
-
Yamal
The West Siberian Super Basin: The largest and most prolific hydrocarbon basin in the world
A Model of the Geological Structure and the Oil and Gas Prospects of Neocomian (Berriasian–Lower Aptian) Sediments of the West Siberia Arctic Regions and the Kara Sea Shelf
Analysis of Water–Gas System Equilibria in Jurassic–Cretaceous Reservoirs (by the Example of the Yamal-Kara Depression)
Geologic structure and correlation of the Berriasian–Lower Aptian productive beds of the Gydan Peninsula ( Russian Arctic )
Tectonic evolution of the Arctic onshore and offshore regions of the West Siberian petroleum province
Seismogeological analysis of the pre-Jurassic sediment complexes of the South Kara syneclise in connection with the tectonic zoning of the sedimentary cover
X-ray computed tomography of two mammoth calf mummies
Abstract The West Siberia basin is the largest petroleum province in Russia, with 80% of the country's gas resources in the Cenomanian Pokur Formation. Significant undiscovered gas resources have been assessed as on trend with the giant gas fields. However, the origin of the large amounts of dry, isotopically light gas is still an enigma, albeit extensively addressed in the literature. This study aims at quantifying the gas contribution from all relevant thermal sources. The West Siberia Basin is the world's largest intracratonic basin, comprising up to 12 km of Mesozoic and Cenozoic clastic rocks. The Basement is composed of Palaeozoic accretionary crust. Northward-trending Permian–Triassic rifts were filled by fluvial–deltaic sediments from the south and east, punctuated by marine transgressions from the north. Cenozoic basin inversion formed traps for petroleum. A regional high-resolution 3D basin simulation was used to model the thermal evolution of the northern West Siberia basin. Geostatistical modelling was applied to assess source rock richness and quality. Basal heat flow was modelled by calibration to bottom-hole temperature and vitrinite measurements. Hydrocarbon generation kinetic parameters were derived from measurements performed on West Siberia rock samples. Thermal gas charge expelled from the hydrocarbon kitchen drainage areas of key fields were compared with the gas volumes accumulated in these fields. The study found that Cretaceous terrestrial sources can generate sufficient early thermal gas to charge accumulations in the South Kara Sea area, and additional Jurassic sources can charge the remaining accumulations of the study area if favourable conditions apply. Biogenic gas is likely to have contributed to the gas accumulations. Mixing of thermal and biogenic gas could explain the observed isotopic composition. Sensitivity analyses show that the timing of structuring and uplift is the most critical factor of the assessment. Variations in glaciation, heat flow and source kinetics show less effect on the hydrocarbon accumulation.