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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Arctic region
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Russian Arctic (1)
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Asia
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Arabian Peninsula
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Oman (1)
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Baikal region (1)
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Indian Peninsula
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India (1)
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Irkutsk Russian Federation (3)
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Krasnoyarsk Russian Federation (8)
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Kuznetsk Basin (1)
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Lena Basin (8)
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Patom Plateau (2)
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Sayan (1)
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Siberia (9)
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Siberian fold belt (2)
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Siberian Platform
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Aldan Shield (2)
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Anabar Shield (2)
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Angara-Lena Basin (3)
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Vilyuy Syneclise (1)
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Yakutia region (1)
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Yenisei Ridge (1)
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Tunguska Basin (23)
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Tunguska Syneclise (1)
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Yakutia Russian Federation
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Anabar Shield (2)
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Olenek River (1)
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Yenisei Basin (2)
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Yenisei-Khatanga basin (1)
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Australasia
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Australia (1)
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Commonwealth of Independent States
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Dnieper Basin (1)
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Russian Federation
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Baikal region (1)
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Irkutsk Russian Federation (3)
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Krasnoyarsk Russian Federation (8)
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Kuznetsk Basin (1)
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Lena Basin (8)
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Patom Plateau (2)
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Russian Arctic (1)
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Siberian Platform
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Aldan Shield (2)
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Anabar Shield (2)
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Angara-Lena Basin (3)
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Vilyuy Syneclise (1)
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Yakutia region (1)
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Yenisei Ridge (1)
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Tunguska Basin (23)
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Tunguska Syneclise (1)
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Yakutia Russian Federation
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Anabar Shield (2)
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Olenek River (1)
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Europe
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Dnieper Basin (1)
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McArthur Basin (1)
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USSR (1)
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commodities
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bitumens
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asphalt (1)
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brines (1)
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diamond deposits (1)
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graphite deposits (1)
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industrial minerals (1)
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metal ores
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iron ores (1)
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mineral deposits, genesis (2)
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nonmetal deposits (1)
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oil and gas fields (3)
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petroleum
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natural gas (1)
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elements, isotopes
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carbon
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C-13/C-12 (6)
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halogens
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chlorine
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Cl-37/Cl-35 (1)
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hydrogen
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D/H (1)
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isotope ratios (7)
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isotopes
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radioactive isotopes
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Rb-87/Sr-86 (1)
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stable isotopes
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C-13/C-12 (6)
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Cl-37/Cl-35 (1)
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D/H (1)
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O-18/O-16 (3)
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Rb-87/Sr-86 (1)
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S-34/S-32 (1)
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Sr-87/Sr-86 (2)
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metals
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alkali metals
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rubidium
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Rb-87/Sr-86 (1)
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alkaline earth metals
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strontium
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Rb-87/Sr-86 (1)
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Sr-87/Sr-86 (2)
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iron (1)
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rare earths (1)
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noble gases
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helium (1)
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oxygen
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O-18/O-16 (3)
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sulfur
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S-34/S-32 (1)
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fossils
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Invertebrata
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Bryozoa (1)
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geochronology methods
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Ar/Ar (1)
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geologic age
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Cenozoic
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Tertiary
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lower Tertiary (1)
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Paleogene
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Paleocene
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lower Paleocene
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K-T boundary (1)
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Mesozoic
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Cretaceous
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Upper Cretaceous
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K-T boundary (1)
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Triassic
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Lower Triassic
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Olenekian (1)
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Permian-Triassic boundary (1)
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Middle Triassic (1)
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Paleozoic
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Cambrian
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Lower Cambrian (2)
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Middle Cambrian (2)
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Carboniferous (1)
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Devonian (2)
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lower Paleozoic (1)
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Ordovician (1)
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Permian
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Lower Permian (1)
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Upper Permian
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Lopingian
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Changhsingian (1)
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Permian-Triassic boundary (1)
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Silurian
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Lower Silurian (2)
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upper Paleozoic (1)
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Precambrian
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upper Precambrian
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Proterozoic
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Neoproterozoic
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Riphean (4)
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Vendian (6)
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igneous rocks
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igneous rocks
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kimberlite (1)
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plutonic rocks
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diabase (4)
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gabbros (1)
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volcanic rocks
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basalts
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trap rocks (2)
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metamorphic rocks
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metamorphic rocks
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marbles (2)
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metasomatic rocks
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skarn (1)
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minerals
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carbonates
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calcite (2)
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spurrite (2)
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native elements
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graphite (2)
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oxides
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silicates
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chain silicates
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wollastonite group
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wollastonite (1)
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framework silicates
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scapolite group
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scapolite (2)
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orthosilicates
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nesosilicates
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garnet group (1)
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merwinite (2)
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olivine group
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monticellite (1)
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spurrite (2)
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sorosilicates
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melilite group
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gehlenite (1)
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sulfates
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anhydrite (1)
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sulfides (2)
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Primary terms
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absolute age (1)
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Arctic region
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Russian Arctic (1)
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Asia
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Arabian Peninsula
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Oman (1)
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Baikal region (1)
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Indian Peninsula
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India (1)
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Irkutsk Russian Federation (3)
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Krasnoyarsk Russian Federation (8)
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Kuznetsk Basin (1)
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Lena Basin (8)
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Patom Plateau (2)
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Sayan (1)
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Siberia (9)
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Siberian fold belt (2)
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Siberian Platform
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Aldan Shield (2)
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Anabar Shield (2)
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Angara-Lena Basin (3)
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Vilyuy Syneclise (1)
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Yakutia region (1)
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Yenisei Ridge (1)
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Tunguska Basin (23)
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Tunguska Syneclise (1)
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Yakutia Russian Federation
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Anabar Shield (2)
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Olenek River (1)
-
-
Yenisei Basin (2)
-
Yenisei-Khatanga basin (1)
-
-
Australasia
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Australia (1)
-
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biogeography (1)
-
bitumens
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asphalt (1)
-
-
brines (1)
-
carbon
-
C-13/C-12 (6)
-
-
Cenozoic
-
Tertiary
-
lower Tertiary (1)
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Paleogene
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Paleocene
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lower Paleocene
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K-T boundary (1)
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crust (1)
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diamond deposits (1)
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Europe
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Dnieper Basin (1)
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explosions (1)
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faults (1)
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geochemistry (5)
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geochronology (1)
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geophysical methods (3)
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graphite deposits (1)
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ground water (2)
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hydrogen
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D/H (1)
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igneous rocks
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kimberlite (1)
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plutonic rocks
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diabase (4)
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gabbros (1)
-
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volcanic rocks
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basalts
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trap rocks (2)
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inclusions
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fluid inclusions (1)
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industrial minerals (1)
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intrusions (6)
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Invertebrata
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Bryozoa (1)
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isotopes
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radioactive isotopes
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Rb-87/Sr-86 (1)
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stable isotopes
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C-13/C-12 (6)
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Cl-37/Cl-35 (1)
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D/H (1)
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O-18/O-16 (3)
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Rb-87/Sr-86 (1)
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S-34/S-32 (1)
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Sr-87/Sr-86 (2)
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lava (1)
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magmas (1)
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Mesozoic
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Cretaceous
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Upper Cretaceous
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K-T boundary (1)
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Triassic
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Lower Triassic
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Olenekian (1)
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Permian-Triassic boundary (1)
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Middle Triassic (1)
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metal ores
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iron ores (1)
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metals
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alkali metals
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rubidium
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Rb-87/Sr-86 (1)
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alkaline earth metals
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strontium
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Rb-87/Sr-86 (1)
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Sr-87/Sr-86 (2)
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iron (1)
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rare earths (1)
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metamorphic rocks
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marbles (2)
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metasomatic rocks
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skarn (1)
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metamorphism (3)
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metasomatism (1)
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Mohorovicic discontinuity (1)
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noble gases
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helium (1)
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nodules (1)
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nonmetal deposits (1)
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oil and gas fields (3)
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oxygen
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O-18/O-16 (3)
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paleoecology (1)
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paleogeography (2)
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Paleozoic
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Cambrian
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Lower Cambrian (2)
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Middle Cambrian (2)
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Carboniferous (1)
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Devonian (2)
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lower Paleozoic (1)
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Ordovician (1)
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Permian
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Lower Permian (1)
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Upper Permian
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Lopingian
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Changhsingian (1)
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Permian-Triassic boundary (1)
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-
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Silurian
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Lower Silurian (2)
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upper Paleozoic (1)
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permafrost (1)
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petroleum
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natural gas (1)
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petrology (1)
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phase equilibria (1)
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pollution (1)
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Precambrian
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upper Precambrian
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Proterozoic
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Neoproterozoic
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Riphean (4)
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Vendian (6)
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sedimentary rocks
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carbonate rocks
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limestone (1)
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chemically precipitated rocks
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evaporites (1)
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clastic rocks
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marl (2)
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sandstone (1)
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-
coal (4)
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-
stratigraphy (1)
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sulfur
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S-34/S-32 (1)
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tectonics (2)
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USSR (1)
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volcanology (1)
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well-logging (1)
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-
rock formations
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Deccan Traps (1)
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Siberian Traps (4)
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-
sedimentary rocks
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sedimentary rocks
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carbonate rocks
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limestone (1)
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chemically precipitated rocks
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evaporites (1)
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-
clastic rocks
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marl (2)
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sandstone (1)
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coal (4)
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-
Tunguska Basin
Carbon and Oxygen Stable Isotopes in Isochemical Contact Metamorphism (Case Study of the Kochumdek Aureole, East Siberia)
Petrology of the Kureika Graphite Deposit in the Roof of the First-Rapid Trap Intrusion (Siberian Platform)
Interaction between Basaltic Melt and Coal Xenoliths in the Trap Intrusion of Mt. Ozernaya (Siberian Platform)
Geochemical Evidence and Geological Prerequisites for Isochemical Metamorphism in the Kochumdek Contact Aureole (East Siberia)
The Vendian–Cambrian Cyclometric Stratigraphic Scale for the Southern and Central Siberian Platform
Field evidence for coal combustion links the 252 Ma Siberian Traps with global carbon disruption: COMMENT
Field evidence for coal combustion links the 252 Ma Siberian Traps with global carbon disruption: REPLY
Disaster microconchids from the uppermost Permian and Lower Triassic lacustrine strata of the Cis-Urals and the Tunguska and Kuznetsk basins (Russia)
Probabilistic Estimation of the Helium Resources in the Central and Southern Areas of the Lena–Tunguska Petroleum Province
Lithology, organic geochemistry, and petroleum potential of the northern areas of the Kureika syneclise
South-Tunguska petroliferous region: geologic structure and petroleum potential
Permafrost and groundwater settings at the site of “Kraton-3” peaceful underground nuclear explosion (Yakutia), from TEM data
Key section of the Preobrazhenka productive horizon in the Vendian–Lower Cambrian carbonate complex ( Lena–Tunguska petroliferous province )
The petroleum accumulation zones in the geological-prospecting regions of the Lena–Tunguska province
Isotopic criteria for predicting the phase composition of hydrocarbons in Riphean and Vendian deposits of the Lena–Tunguska petroleum province
Abstract The Siberian craton consists of crystalline rocks and superimposed Precambrian sedimentary rocks deposited in rift basins. Palaeozoic rocks, mainly carbonates, were deposited along the margins of the craton to form an outwardly younger concentric pattern that underlies an outward-thickening Mesozoic sedimentary section. The north and east margins of the Siberian craton subsequently became foreland basins created by compressional deformation during collision with other tectonic plates. The Tunguska Basin developed as a Palaeozoic rift/sag basin over Proterozoic rifts. The geological provinces along the north and east margins of the Siberian craton are immature with respect to exploration, so exploration-history analysis alone cannot be used for assessing undiscovered petroleum resources. Therefore, other areas from around the world having greater petroleum exploration maturity and similar geological characteristics, and which have been previously assessed, were used as analogues to aid in this assessment. The analogues included those of foreland basins and rift/sag basins that were later subjected to compression. The US Geological Survey estimated the mean undiscovered, technically recoverable conventional petroleum resources to be c. 28 billion barrels of oil equivalent, including c. 8 billion barrels of crude oil, 103 trillion cubic feet of natural gas, and 3 billion barrels of natural gas liquids.