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all geography including DSDP/ODP Sites and Legs
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Arctic Ocean
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Chukchi Sea (1)
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Kara Sea (1)
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Arctic region
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Asia
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Altai Russian Federation
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Gorny Altai (10)
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Altai-Sayan region (10)
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Baikal region (3)
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Central Asia
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Kazakhstan
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Alakol (1)
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Far East
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China
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Atlantic Ocean
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Commonwealth of Independent States
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Kalba Range (1)
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Zaisan Basin (1)
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Zaisan Kazakhstan (1)
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Kulunda Steppe (1)
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Rudny Altai (3)
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Russian Federation
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Arkhangelsk Russian Federation
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Novaya Zemlya (1)
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Baikal region (3)
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Kemerovo Russian Federation
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Okhotsk-Chukchi volcanic belt (1)
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Russian Arctic
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Salair Ridge (3)
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Urals
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Caucasus
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Timan Ridge (1)
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Variscides (2)
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Pacific region
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Russian Platform
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Timan Ridge (1)
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commodities
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Nd-144/Nd-142 (1)
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stable isotopes
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Ar-40/Ar-39 (1)
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He-4/He-3 (1)
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Hf-177/Hf-176 (4)
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Nd-144/Nd-142 (1)
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Nd-144/Nd-143 (9)
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O-17/O-16 (1)
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O-18/O-16 (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 (5)
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Lu/Hf (1)
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rubidium
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alkaline earth metals
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magnesium (1)
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Sr-87/Sr-86 (5)
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antimony (1)
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Nd-144/Nd-142 (1)
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Nd-144/Nd-143 (9)
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Sm-147/Nd-144 (1)
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samarium
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silver (1)
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noble gases
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Ar-40/Ar-39 (1)
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helium
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oxygen
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O-17/O-16 (1)
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O-18/O-16 (2)
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sulfur
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S-34/S-32 (1)
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Chordata
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Vertebrata (1)
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Graptolithina (1)
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Invertebrata
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Protista
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Conodonta (1)
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Pterobranchia (1)
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geochronology methods
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Ar/Ar (9)
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Cenozoic
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Tertiary
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Neogene
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Miocene (1)
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Mesozoic
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Cretaceous
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Paleozoic
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Carboniferous
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Devonian
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lower Paleozoic (3)
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Upper Ordovician
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Permian
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Permian-Triassic boundary (1)
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upper Paleozoic (11)
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Phanerozoic (1)
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Precambrian
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upper Precambrian
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Proterozoic
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granosyenite (1)
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ultramafics
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peridotites (2)
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volcanic rocks
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basalts
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mid-ocean ridge basalts (2)
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tholeiite (1)
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dacites (2)
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pyroclastics
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rhyolites
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quartz porphyry (1)
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ophiolite (3)
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metamorphic rocks
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amphibolites (2)
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eclogite (1)
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gneisses
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biotite gneiss (1)
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metaigneous rocks
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metabasalt (2)
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pyroxene group
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framework silicates
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silica minerals
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quartz (2)
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orthosilicates
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garnet group (2)
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olivine (1)
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sillimanite (1)
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staurolite (1)
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zircon group
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zircon (16)
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sheet silicates
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mica group
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biotite (4)
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muscovite (3)
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sericite (1)
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sulfides (1)
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Primary terms
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absolute age (22)
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Arctic Ocean
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Barents Sea (1)
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Chukchi Sea (1)
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Kara Sea (1)
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Laptev Sea (1)
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Arctic region
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Novaya Zemlya (1)
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Asia
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Altai Mountains
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Gorny Altai (10)
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Kalba Range (1)
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Kuznetsk Alatau (2)
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Mongolian Altai (3)
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Altai Russian Federation
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Gorny Altai (10)
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Altai-Sayan region (10)
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Baikal region (3)
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Central Asia
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Kazakhstan
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Alakol (1)
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Central Kazakhstan (1)
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Eastern Kazakhstan
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Chingis-Tau (1)
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Kalba Range (1)
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Kokchetav Kazakhstan
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Kokchetav Massif (3)
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Zaisan Basin (1)
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Zaisan Kazakhstan (1)
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Pamirs (1)
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Far East
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China
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Gansu China (1)
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North China Platform (1)
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Tarim Platform (2)
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Xinjiang China
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Junggar (6)
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Junggar Basin (1)
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Tarim Basin (2)
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Turpan Basin (1)
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Mongolia
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Hangay Mountains (2)
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Mongolian Altai (3)
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Himalayas (1)
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Kemerovo Russian Federation
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Krasnoyarsk Russian Federation (1)
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Kulunda Steppe (1)
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Kuznetsk Basin (2)
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Lake Baikal (1)
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Novosibirsk Russian Federation (3)
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Okhotsk-Chukchi volcanic belt (1)
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Omsk Russian Federation (1)
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Rudny Altai (3)
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Salair Ridge (3)
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Sayan
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Western Sayan (2)
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Siberia (9)
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Siberian Platform
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Yenisei Ridge (1)
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Sikhote-Alin Range (1)
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Tarbagatay Range (1)
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Tien Shan (5)
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Tomsk Russian Federation (2)
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Tuva Russian Federation (3)
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West Siberia
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Kuznetsk Alatau (2)
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Yakutia Russian Federation
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New Siberian Islands (1)
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Yenisei Basin (1)
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Atlantic Ocean
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North Atlantic (1)
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Cenozoic
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Tertiary
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Neogene
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Miocene (1)
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Pliocene
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upper Pliocene (1)
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-
-
Paleogene
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Oligocene (2)
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upper Cenozoic (1)
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Chordata
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Vertebrata (1)
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continental drift (1)
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crust (10)
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deformation (9)
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Eurasia (2)
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Europe
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Arkhangelsk Russian Federation
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Novaya Zemlya (1)
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Caucasus
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Northern Caucasus (1)
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Timan Ridge (1)
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Variscides (2)
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faults (16)
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folds (3)
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foliation (3)
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geochemistry (4)
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geochronology (4)
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geomorphology (1)
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geophysical methods (5)
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Graptolithina (1)
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heat flow (2)
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Hemichordata (1)
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igneous rocks
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peperite (1)
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picrite (3)
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plutonic rocks
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diabase (3)
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diorites
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plagiogranite (3)
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quartz diorites (2)
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tonalite (1)
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gabbros
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norite (1)
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troctolite (1)
-
-
granites
-
alaskite (1)
-
aplite (1)
-
A-type granites (1)
-
biotite granite (1)
-
granite porphyry (1)
-
granosyenite (1)
-
leucogranite (1)
-
-
lamprophyres
-
spessartite (1)
-
-
monzonites (1)
-
pegmatite (1)
-
syenites
-
granosyenite (1)
-
-
ultramafics
-
peridotites (2)
-
-
-
volcanic rocks
-
andesites
-
boninite (1)
-
-
basalts
-
mid-ocean ridge basalts (2)
-
tholeiite (1)
-
-
dacites (2)
-
pyroclastics
-
tuff (1)
-
-
rhyolites
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quartz porphyry (1)
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inclusions
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fluid inclusions (2)
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intrusions (15)
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Invertebrata
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Protista
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Radiolaria (1)
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isotopes
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radioactive isotopes
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Ar-40/Ar-39 (1)
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Nd-144/Nd-142 (1)
-
Rb-87/Sr-86 (1)
-
Sm-147/Nd-144 (1)
-
-
stable isotopes
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Ar-40/Ar-39 (1)
-
He-4/He-3 (1)
-
Hf-177/Hf-176 (4)
-
Nd-144/Nd-142 (1)
-
Nd-144/Nd-143 (9)
-
O-17/O-16 (1)
-
O-18/O-16 (2)
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Rb-87/Sr-86 (1)
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S-34/S-32 (1)
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Sm-147/Nd-144 (1)
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Sr-87/Sr-86 (5)
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lava (2)
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lineation (2)
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magmas (7)
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mantle (10)
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Mesozoic
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Cretaceous
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Lower Cretaceous
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Albian (1)
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Jurassic
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lower Mesozoic (2)
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Triassic
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metal ores
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lead ores (1)
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silver ores (1)
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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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magnesium (1)
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strontium
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Rb-87/Sr-86 (1)
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Sr-87/Sr-86 (5)
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antimony (1)
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arsenic (1)
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gold (2)
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hafnium
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Hf-177/Hf-176 (4)
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iron (1)
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mercury (1)
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niobium (1)
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platinum group (2)
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rare earths
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neodymium
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Nd-144/Nd-142 (1)
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Nd-144/Nd-143 (9)
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Sm-147/Nd-144 (1)
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samarium
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Sm-147/Nd-144 (1)
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silver (1)
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metamorphic rocks
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amphibolites (2)
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eclogite (1)
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gneisses
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biotite gneiss (1)
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metaigneous rocks
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metabasalt (2)
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serpentinite (1)
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metasedimentary rocks
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metapelite (1)
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metasomatic rocks
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serpentinite (1)
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migmatites (2)
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mylonites (2)
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metamorphism (6)
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metasomatism (3)
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Mohorovicic discontinuity (1)
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noble gases
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argon
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Ar-40/Ar-39 (1)
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helium
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He-4/He-3 (1)
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1-20 OF 69 RESULTS FOR
Ob-Zaisan Ocean
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Journal Article
Late Paleozoic closure of the Ob-Zaisan Ocean along the Irtysh shear zone (NW China): Implications for arc amalgamation and oroclinal bending in the Central Asian orogenic belt
Journal: GSA Bulletin
Publisher: Geological Society of America
Published: 01 May 2017
GSA Bulletin (2017) 129 (5-6): 547–569.
..., thus allowing us to map the exact location of the tectonic boundary. Detrital zircon data constrain the initial closure of the Ob-Zaisan Ocean to the late Carboniferous (<323 Ma), and new structural and 40 Ar/ 39 Ar geochronological data shed light on the subsequent collisional processes. We propose...
Journal Article
Problems of geodynamics, tectonics, and metallogeny of orogens
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 December 2011
Russ. Geol. Geophys. (2011) 52 (12): 1505–1515.
...-slip faulting. Plume magmatism was an active agent in ocean opening when the Paleotethys, Ural, Ob–Zaisan, and Turkestan basins appeared while the Late Cambrian–Ordovician orogen was forming in Central Asia (North Kazakhstan, Altai–Sayan, Tuva, and Baikal areas). Closure of the Ob–Zaisan ocean...
Journal Article
Tectonics and geodynamics of the Central Asian Foldbelt: the role of Late Paleozoic large-amplitude strike-slip faults
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 January 2011
Russ. Geol. Geophys. (2011) 52 (1): 52–71.
... and formation of the composite-continent basement. In Late Cambrian and Early Ordovician, this continent was separated from Siberia by the Ob’–Zaisan ocean basin. (2) The Vendian and Paleozoic Siberian continental margin complexes comprising the Vendian–Cambrian Kuznetsk–Altai island arc and the rock complexes...
Journal Article
Late Paleozoic Accretionary and Collisional Processes along the Southern Peri-Siberian Orogenic System: New Constraints from Amphibolites within the Irtysh Complex of Chinese Altai
Journal: The Journal of Geology
Publisher: The University of Chicago Press
Published: 01 March 2019
The Journal of Geology (2019) 127 (2): 241–262.
... relicts of the Ob-Zaisan Ocean between the peri-Siberian and Kazakhstan-Junggar orogenic systems. In contrast, ankaramites from the Dulate arc of East Junggar or chemical equivalents possibly served as the protoliths of type III amphibolites. 2. The Irtysh Complex represents an accretionary prism...
Includes: Supplemental Content
Journal Article
Tectonics and geodynamics of Gorny Altai and adjacent structures of the Altai–Sayan folded area
M.M. Buslov, H. Geng, A.V. Travin, D. Otgonbaatar, A.V. Kulikova, Chen Ming, G. Stijn, N.N. Semakov, E.S. Rubanova, M.A. Abildaeva, E.E. Voitishek, D.A. Trofimova
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 October 2013
Russ. Geol. Geophys. (2013) 54 (10): 1250–1271.
..., they were separated by the Ob’–Zaisan oceanic basin, whose fragments are preserved in the Caledonian suture-shear zone. The movements during the Late Paleozoic occurred along older, reactivated structures and produced the large intracontinental Central Asian orogen, which is interpreted to be a far-field...
Journal Article
Tectonics and geodynamics of the western Central Asian Fold Belt ( Kazakhstan Paleozoides )
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 December 2011
Russ. Geol. Geophys. (2011) 52 (12): 1600–1618.
... in the Silurian. The Sakmarian, Tagil, Eastern Urals, and Stepnyak volcanic arcs formed at the boundaries with the Ural, Turkestan, and Junggar–Balkhash Oceans. In the late Silurian, Kazakhstania collided with the island arcs of the Turkestan and Ob’–Zaisan Oceans, with the formation of molasse and granite belts...
Image
a , Paleogeographic reconstruction diagram (modified after Filippova et al....
in Late Paleozoic Accretionary and Collisional Processes along the Southern Peri-Siberian Orogenic System: New Constraints from Amphibolites within the Irtysh Complex of Chinese Altai
> The Journal of Geology
Published: 01 March 2019
Orogen, as part of the peri-Siberia orogenic system, was under subduction of the intervening Ob-Zaisan Ocean (i.e., a branch of the PAO) between this orogenic system and the Kazakhstan-Junggar orogenic collage. BL = Barlyk arc; ChTS = Chinese Tien Shan; CTS = Central Tien Shan; KHM = Khanty-Mansi; MG
Image
Tentative tectonic reconstruction of the western Central Asian orogenic bel...
in Late Paleozoic closure of the Ob-Zaisan Ocean along the Irtysh shear zone (NW China): Implications for arc amalgamation and oroclinal bending in the Central Asian orogenic belt
> GSA Bulletin
Published: 01 May 2017
the closure of the Ob-Zaisan Ocean (modified after P. Li et al., 2015a ). DVB—Devonian volcanic belt; CKF—Central Kazakhstan fault; ISZ—Irtysh shear zone; CANTF—Chingiz–Alakol–North Tian Shan fault; MTSZ—Main Tianshan shear zone.
Journal Article
Early Paleozoic tectonics and geodynamics of Central Asia: role of mantle plumes
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 December 2011
Russ. Geol. Geophys. (2011) 52 (12): 1539–1552.
... into the Kazakhstan–Tuva–Mongolia system. The formation of the Late Cambrian–Ordovician orogen in Central Asia was synchronous with opening of the Ural, Ob–Zaisan, Turkestan, and Paleotethys oceans. The plume pulses (520–500 and 490–460 Ma) may have been responsible for opening of new oceans, accelerated amalgamation...
Journal Article
MAJOR EPOCHS OF INTRUSIVE MAGMATISM OF KUZNETSK ALATAU, ALTAI, AND KALBA ( from U-Pb isotope dates )
A. G. Vladimirov, M. S. Kozlov, S. P. Shokal’skii, V. A. Khalilov, S. N. Rudnev, N. N. Kruk, S. A. Vystavnoi, S. M. Borisov, Yu. K. Bereziko, A. N. Metsner, G. A. Babin, A. N. Mamlin, O. M. Murzin, G. V. Nazarov, V. A. Makarov
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 August 2001
Russ. Geol. Geophys. (2001) 42 (8): 1089–1109.
... of active continental margin of the Andean type; C 1 v-C 3 – accretion-collisional, related to the oblique collision of the Dzhungar microplate with the Siberian continent and closure of the Ob’-Zaisan paleoocean basin; P 1 -T 2 – postcollisional, realized in the strike-slip motion regime; and T 3 -J 1...
Journal Article
Basic and Associated Granitoid Magmatism and Geodynamic Evolution of the Altai Accretion–Collision System (Eastern Kazakhstan)
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 March 2022
Russ. Geol. Geophys. (2022) 63 (3): 279–299.
...” was introduced for such orogens ( Khain et al., 1996 ; Vladimirov et al., 2003 ). The general sequence of geodynamic events in the study area of the Ob’–Zaisan folded system is as follows: subduction → convergence of continental blocks and reduction in the ocean basin → termination of marine sedimentation...
Image
Schematic illustration of the tectonic evolution of the Kazakhstan-Tien Sha...
Published: 01 August 2014
in the back-arc riftogenic setting in the Ob’-Zaisan back-arc basin. (b) Middle Paleozoic: back-arc rifting was followed by opening of the Ob’-Zaissan back-arc oceanic basin. (c) Devonian: the onset of subduction in this oceanic basin under the Altai-Mongol superterrane initiated arc magmatism in the Rudny
Journal Article
LATE PALEOZOIC, MIDDLE MESOZOIC, AND LATE CENOZOIC STAGES OF THE ALTAI OROGENY
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 May 2002
Russ. Geol. Geophys. (2002) 43 (5): 434–445.
... stages [ 21 ]. The geological history of the adjacent Chinese territory was suggested to include a Yanshan (Mesozoic) and a Himalayan (Cenozoic) stages of tectonic activity. In the Early Carboniferous, the Ob’-Zaisan Hercynian ocean went through the final stage of its evolution. It closed...
Image
The Vendian-Cambrian island arc fragments in the framework of the Siberian ...
in FRAGMENTS OF OCEANIC ISLANDS IN THE KURAI AND KATUN’ ACCRETIONARY WEDGES OF GORNY ALTAI
> Russian Geology and Geophysics
Published: 01 December 2004
Fig. 3. The Vendian-Cambrian island arc fragments in the framework of the Siberian continent [ 18 ]. 1 — Cenozoic depression; 2 — Hercynides of the Ob’-Zaisan and Tom’-Kolyvan’ folded area; 3 — microcontinents: Tuva-Mongolian (TM), Barguzin (B), Altai-Mongolian (AM), 4 — Siberian
Journal Article
Geology and mineralogy of East Kazakhstan gold-bearing jasperoids ( by the example of the Baybura ore field )
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 December 2013
Russ. Geol. Geophys. (2013) 54 (12): 1471–1483.
... of the Altai Hercynides is now interpreted in terms of the gradual convergence of the Kazakhstan and Siberian Plates during their clockwise rotation relative to each other and the simultaneous reduction of the Ob’–Zaisan paleo-ocean basin (D 1–2 –C 1 ). At that time, the Ob’–Zaisan basin interacted...
Journal Article
URALIDES AND TIMANIDES: THEIR STRUCTURAL RELATIONSHIP AND POSITION IN THE GEOLOGIC HISTORY OF THE URAL-MONGOLIAN FOLD BELT
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 January 2003
Russ. Geol. Geophys. (2003) 44 (1-2): 28–39.
.... In the Carboniferous the structures of the Ural-Mongolian belt agglomerated. At that time, the Kazakhstanian continent was pushed into the oceanic space between Baltica and Siberia, and their joint collision began, which led to the formation of the Valerianovka and Ob’-Zaisan suture zones in the late Early...
Journal Article
EVOLUTION OF STRUCTURES OF THE URALS, KAZAKHSTAN, TIEN SHAN, AND ALTAI-SAYAN REGION WITHIN THE URAL-MONGOLIAN FOLD BELT ( Paleoasian Ocean )
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 January 2003
Russ. Geol. Geophys. (2003) 44 (1-2): 5–27.
...-Tethys. An immediate contact of the paleo-Tethys and Paleoasian structures is observed in the southern Tien Shan (see below). Relationships between the paleo-Tethys and late stages of the Paleoasian ocean (Uralian and Ob’-Junggar paleo-oceans, which appeared in the Ordovician) are a special problem...
Journal Article
Permian magmatism and lithospheric deformation in the Altai caused by crustal and mantle thermal processes
A.G. Vladimirov, N.N. Kruk, S.V. Khromykh, O.P. Polyansky, V.V. Chervov, V.G. Vladimirov, A.V. Travin, G.A. Babin, M.L. Kuibida, V.D. Khomyakov
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 July 2008
Russ. Geol. Geophys. (2008) 49 (7): 468–479.
... of classical tectonics, the area coincides with the Zaisan folded area produced by closure of the Char paleo-ocean in the Late Carboniferous. However, the extent, structure, and composition of magmatism at the Carboniferous-Permian (280±10 Ma) and Permian-Triassic (250±5 Ma) boundaries require an active...
Journal Article
Interplay of magmatism, sedimentation, and collision processes in the Siberian craton and the flanking orogens
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 October 2013
Russ. Geol. Geophys. (2013) 54 (10): 1135–1149.
..., Mongolia, Kazakhstan, and Tien Shan, and its crust consists of both juvenile and recycled material ( Kovach et al., 2013 ). In the Early–Middle Paleozoic, the continent was separated from Siberia by the Ob‘–Zaisan ocean. The Vendian–Early Paleozoic Charysh–Terekta–Ulagan–Sayan–Olkhon strike-slip suture...
Journal Article
PETROLOGY OF THE KUOLOTONG SULFIDE COPPER-NICKEL DEPOSIT IN NORTHWESTERN CHINA
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 November 2011
Russ. Geol. Geophys. (2002) 43 (11): 990–1001.
...-bearing picrite-dolerite formation are widespread in the Hercynian structures of the Zaisan-Gobi fold belt, extending from the Ob’ basin (Novosibirsk region) through East Kazakhstan and North Xinjiang to the Gobi segment of the Hercynides of South Mongolia [ 1 ]. In the Zaisan and Gobi segments...
1