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NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
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Asia
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Altai-Sayan region (1)
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Arabian Peninsula
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Oman (1)
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Baikal Mountains (2)
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Baikal region (6)
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Buryat Russian Federation (1)
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Irkutsk Russian Federation
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Bodaibo Russian Federation (1)
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Khabarovsk Russian Federation (1)
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Krasnoyarsk Russian Federation
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Igarka Russian Federation (1)
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Turukhansk Russian Federation (1)
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Lake Baikal (1)
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Lena Basin (3)
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Maya River basin (1)
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Olekma River (1)
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Patom Plateau (18)
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Siberia (8)
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Siberian fold belt (4)
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Siberian Platform
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Aldan Shield (1)
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Anabar Shield (1)
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Angara-Lena Basin (2)
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Vilyuy Syneclise (2)
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Yenisei Ridge (3)
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Tunguska Basin (2)
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Tuva Russian Federation
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Sangilen Mountains (1)
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Uchur River basin (1)
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Vilyuy River basin (1)
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Yakutia Russian Federation
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Anabar Shield (1)
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Verkhoyansk Range (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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Caledonides (1)
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Canada
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Western Canada
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Northwest Territories (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 Mountains (2)
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Baikal region (6)
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Buryat Russian Federation (1)
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Irkutsk Russian Federation
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Bodaibo Russian Federation (1)
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-
Khabarovsk Russian Federation (1)
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Krasnoyarsk Russian Federation
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Igarka Russian Federation (1)
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Turukhansk Russian Federation (1)
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-
Lake Baikal (1)
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Lena Basin (3)
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Maya River basin (1)
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Olekma River (1)
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Patom Plateau (18)
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Siberian Platform
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Aldan Shield (1)
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Anabar Shield (1)
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Angara-Lena Basin (2)
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Vilyuy Syneclise (2)
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Yenisei Ridge (3)
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-
Tunguska Basin (2)
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Tuva Russian Federation
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Sangilen Mountains (1)
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Uchur River basin (1)
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Vilyuy River basin (1)
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Yakutia Russian Federation
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Anabar Shield (1)
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Verkhoyansk Range (1)
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Europe
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Dnieper Basin (1)
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Variscides (1)
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Franklin Mountains (1)
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McArthur Basin (1)
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North America
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Canadian Shield
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Churchill Province
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Cape Smith fold belt (1)
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commodities
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bitumens (1)
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diamond deposits (1)
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metal ores
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copper ores (1)
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gold ores (4)
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nickel ores (1)
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platinum ores (2)
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mineral deposits, genesis (4)
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petroleum (4)
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placers (1)
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elements, isotopes
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carbon
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C-13/C-12 (2)
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halogens
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chlorine (1)
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isotope ratios (3)
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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 (2)
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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 (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 (1)
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platinum group
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palladium (1)
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platinum (1)
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platinum ores (2)
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precious metals (1)
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rare earths (1)
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sulfur
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S-34/S-32 (1)
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fossils
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microfossils (2)
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palynomorphs
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acritarchs (1)
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geochronology methods
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Ar/Ar (1)
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U/Pb (1)
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geologic age
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Cenozoic (1)
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Mesozoic (1)
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Paleozoic
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Cambrian
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Lower Cambrian
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Yudoma Series (1)
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lower Paleozoic (2)
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Precambrian
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upper Precambrian
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Proterozoic
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Mesoproterozoic (1)
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Neoproterozoic
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Cryogenian (1)
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Ediacaran (4)
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Riphean
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upper Riphean (1)
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Vendian (5)
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igneous rocks
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igneous rocks
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kimberlite (1)
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picrite (1)
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plutonic rocks
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gabbros (1)
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granites (1)
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ultramafics
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peridotites
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dunite (1)
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pyroxenite (1)
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volcanic rocks (1)
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metamorphic rocks
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metamorphic rocks
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phyllites (1)
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schists
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greenschist (1)
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minerals
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native elements (1)
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silicates
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framework silicates
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silica minerals
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quartz (1)
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sulfides
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pyrite (2)
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Primary terms
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absolute age (2)
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Asia
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Altai-Sayan region (1)
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Arabian Peninsula
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Oman (1)
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Baikal Mountains (2)
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Baikal region (6)
-
Buryat Russian Federation (1)
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Irkutsk Russian Federation
-
Bodaibo Russian Federation (1)
-
-
Khabarovsk Russian Federation (1)
-
Krasnoyarsk Russian Federation
-
Igarka Russian Federation (1)
-
Turukhansk Russian Federation (1)
-
-
Lake Baikal (1)
-
Lena Basin (3)
-
Maya River basin (1)
-
Olekma River (1)
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Patom Plateau (18)
-
Siberia (8)
-
Siberian fold belt (4)
-
Siberian Platform
-
Aldan Shield (1)
-
Anabar Shield (1)
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Angara-Lena Basin (2)
-
Vilyuy Syneclise (2)
-
Yenisei Ridge (3)
-
-
Tunguska Basin (2)
-
Tuva Russian Federation
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Sangilen Mountains (1)
-
-
Uchur River basin (1)
-
Vilyuy River basin (1)
-
Yakutia Russian Federation
-
Anabar Shield (1)
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Verkhoyansk Range (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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biogeography (1)
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bitumens (1)
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Canada
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Western Canada
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Northwest Territories (1)
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-
-
carbon
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C-13/C-12 (2)
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Cenozoic (1)
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chemical analysis (1)
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crust (3)
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deformation (1)
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diamond deposits (1)
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earthquakes (1)
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Europe
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Dnieper Basin (1)
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Variscides (1)
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faults (4)
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folds (1)
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geochemistry (2)
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igneous rocks
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kimberlite (1)
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picrite (1)
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plutonic rocks
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gabbros (1)
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granites (1)
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ultramafics
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peridotites
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dunite (1)
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pyroxenite (1)
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-
-
volcanic rocks (1)
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-
intrusions (1)
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isotopes
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radioactive isotopes
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Rb-87/Sr-86 (1)
-
-
stable isotopes
-
C-13/C-12 (2)
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Rb-87/Sr-86 (1)
-
S-34/S-32 (1)
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Sr-87/Sr-86 (1)
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magmas (1)
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mantle (1)
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Mesozoic (1)
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metal ores
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copper ores (1)
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gold ores (4)
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nickel ores (1)
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platinum ores (2)
-
-
metals
-
alkali metals
-
rubidium
-
Rb-87/Sr-86 (1)
-
-
-
alkaline earth metals
-
strontium
-
Rb-87/Sr-86 (1)
-
Sr-87/Sr-86 (1)
-
-
-
platinum group
-
palladium (1)
-
platinum (1)
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platinum ores (2)
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precious metals (1)
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rare earths (1)
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-
metamorphic rocks
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phyllites (1)
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schists
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greenschist (1)
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metamorphism (2)
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mineral deposits, genesis (4)
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Mohorovicic discontinuity (1)
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North America
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Canadian Shield
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Churchill Province
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Cape Smith fold belt (1)
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paleogeography (1)
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Paleozoic
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Cambrian
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Lower Cambrian
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Yudoma Series (1)
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lower Paleozoic (2)
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palynomorphs
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acritarchs (1)
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paragenesis (1)
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petroleum (4)
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placers (1)
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plate tectonics (3)
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Precambrian
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upper Precambrian
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Proterozoic
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Mesoproterozoic (1)
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Neoproterozoic
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Cryogenian (1)
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Ediacaran (4)
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Riphean
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upper Riphean (1)
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Vendian (5)
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sea water (1)
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sedimentary rocks
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carbonate rocks (1)
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chemically precipitated rocks
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evaporites (1)
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phosphate rocks (1)
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weathering crust (1)
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clastic rocks
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black shale (3)
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mudstone (1)
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shale (1)
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sedimentation (1)
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structural analysis (1)
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sulfur
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S-34/S-32 (1)
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tectonics
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neotectonics (1)
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weathering (1)
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sedimentary rocks
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sedimentary rocks
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carbonate rocks (1)
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chemically precipitated rocks
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evaporites (1)
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phosphate rocks (1)
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weathering crust (1)
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clastic rocks
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black shale (3)
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mudstone (1)
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shale (1)
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Patom Plateau
Geodynamic Characteristics of Neotectonic Structures in the Olenek and Vilyui Areas of the Yakutian Kimberlite Province
Chapter 25: The Sukhoi Log Gold Deposit, Russia
Abstract Sukhoi Log, Russia’s largest gold deposit, containing 1,960 metric tons (t) of gold within the deformed Neoproterozoic sedimentary sequences of the Patom passive margin, can be classified as an orogenic gold system. This giant and nearby smaller deposits occur in black shale horizons at several stratigraphic levels. The understanding of Sukhoi Log evolved from a small quartz vein occurrence to a large disseminated gold resource. The genesis of the deposit, originally considered to be related to a granitic intrusion, was later reinterpreted as metamorphogenic, with a significant contribution of synsedimentary gold in pyrite. Recent isotopic studies showed that there may have been more than one early Paleozoic synmetamorphic gold-mineralizing event, so the deposit most likely has a multistage origin. Black shales might have acted either as a synsedimentary and/or synmetamorphic geochemical trap for auriferous fluids. Structurally, the mineralization is confined to the axial portion of the recumbent Sukhoi Log anticline, conjugate with the Kadali-Sukhoi Log shear zone. This imbricate thrust zone marks a major boundary between the Chuya-Nechera anticlinorium and Bodaibo synclinorium, two regional tectonic features in the Patom Highlands.
C and Sr isotope chemostratigraphy of Vendian–Lower Cambrian carbonate sequences in the central Siberian Platform
Geochemistry of organic matter of the Neoproterozoic strata within the Berezovka depression ( Seralakh Formation, Siberian Platform )
Ultramafic–mafic igneous complexes of the Precambrian East Siberian metallogenic province ( southern framing of the Siberian craton ): age, composition, origin, and ore potential
Ediacaran Microfossils from the Ura Formation, Baikal-Patom Uplift, Siberia: Taxonomy and Biostratigraphic Significance
Tectonic map of the Vendian–Lower Paleozoic structural stage of the Lena–Tunguska petroleum province, Siberian Platform
Identifying paleorifts as promising tectonic elements for active oil and gas generation
Sulfur isotopes in sediment-hosted orogenic gold deposits: Evidence for an early timing and a seawater sulfur source
Fissured quartz and the problem of study of pre-Riphean metamorphosed residual crust of weathering on the Chuya-Nechera granites of the Patom upland
We discuss the Late Neoproterozoic and Vendian and Cambrian evolution of sedimentary basins and regional deposition events in the southwestern and southern margins of the Siberian craton from the Igarka region in the lower reaches of the Yenisei to the Patom Upland northeast of Lake Baikal. The deposition history between ca. 750 and 543 Ma was reconstructed using correlation of Late Neoproterozoic sediments with regard to diamictite deposited during global Sturtian and Varangerian glacials, rifting and collisional events, and eustatic sea level fluctuations. The accretionary and collisional events of 880–750 Ma were followed by the breakup of the supercontinent that included Siberia and the inception of failed rifts in the territory of the Yenisei Ridge, the Sayan and Baikal regions, and the Patom Upland. The main rifting stage was associated with the formation of the passive continental margin and high-energy tidal deposition on widespread broad shelves. The earliest Vendian (Ediacaran) was marked by the onset of another accretionary stage when marine deposition was disturbed by regional-scale continental glaciation (the Varangerian glacial epoch) and deep exaration of Late Riphean shelves. Vendian climate and tectonic events are reflected in the evolution of a peripheral foreland basin on the craton margin that went through several stages: (1) Early–Late Vendian subduction, glaciation, and then terrigenous carbonate shelf deposition (ca. 600 Ma). Subduction was accompanied by transgression of the fringing seas onto the craton and centrifugal transport of clastics. (2) Late Vendian collision and accretion, growth of bordering orogens, and continental molasse deposition (ca. 550 Ma). The collisional processes interrupted the marine deposition of the previous stage, closed the remnant marginal basins, and produced a peripheral orogen of a great extent. Deposition was on broad alluvial plains, and clastics were transported centripetally. (3) Late Vendian–Early Cambrian rifting and subsidence of a hangingwall clastic basin (ca. 543 Ma). Plate reorganization caused extension and related rifting and doming on the craton. The hangingwall basin on the slopes of domes received clastics from new sources on the uplifted basement blocks on the craton periphery. The dispersal of the collision-accretionary collage (the Vendian Pannotia continent) was completed in the Early–Middle Cambrian by the formation of carbonate platforms and an evaporite basin.