Skip Nav Destination
Close Modal
RESULTS FOR
Beshcheul' Formation
Update search
Filter
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
Filter
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
Filter
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
Filter
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
Filter
- Abstract
- Affiliation
- All
- Authors
- Book Series
- DOI
- EISBN
- EISSN
- Full Text
- GeoRef ID
- ISBN
- ISSN
- Issue
- Keyword (GeoRef Descriptor)
- Meeting Information
- Report #
- Title
- Volume
Filter
- 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
Format
Article Type
Journal
Publisher
Section
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
-
Asia
-
Buryat Russian Federation
-
Vitim Plateau (1)
-
-
Central Asia
-
Turgay Basin (1)
-
-
Irtysh River (2)
-
Krasnoyarsk Russian Federation (1)
-
Kulunda Steppe (1)
-
Kurgan Russian Federation (1)
-
Novosibirsk Russian Federation (5)
-
Ob-Irtysh Interfluve (1)
-
Omsk Russian Federation (5)
-
Tomsk Russian Federation (2)
-
Tyumen Russian Federation (1)
-
West Siberia
-
Siberian Lowland (2)
-
-
Western Transbaikalia (1)
-
-
Commonwealth of Independent States
-
Kulunda Steppe (1)
-
Ob-Irtysh Interfluve (1)
-
Russian Federation
-
Buryat Russian Federation
-
Vitim Plateau (1)
-
-
Krasnoyarsk Russian Federation (1)
-
Kurgan Russian Federation (1)
-
Novosibirsk Russian Federation (5)
-
Omsk Russian Federation (5)
-
Tomsk Russian Federation (2)
-
Tyumen Russian Federation (1)
-
Western Transbaikalia (1)
-
-
West Siberia
-
Siberian Lowland (2)
-
-
-
-
elements, isotopes
-
carbon
-
C-13/C-12 (2)
-
C-14 (1)
-
-
hydrogen
-
D/H (2)
-
-
isotope ratios (2)
-
isotopes
-
radioactive isotopes
-
C-14 (1)
-
Rn-222 (1)
-
-
stable isotopes
-
C-13/C-12 (2)
-
D/H (2)
-
O-18/O-16 (2)
-
-
-
metals
-
actinides
-
thorium (1)
-
uranium (1)
-
-
alkaline earth metals
-
radium (1)
-
-
rare earths (1)
-
-
noble gases
-
radon
-
Rn-222 (1)
-
-
-
oxygen
-
dissolved oxygen (1)
-
O-18/O-16 (2)
-
-
trace metals (1)
-
-
fossils
-
Chordata
-
Vertebrata
-
Tetrapoda
-
Mammalia
-
Theria
-
Eutheria
-
Rodentia
-
Myomorpha
-
Cricetidae
-
Microtus (1)
-
-
-
-
-
-
-
-
-
-
eukaryotes (1)
-
Invertebrata
-
Mollusca (1)
-
-
microfossils (6)
-
palynomorphs
-
Dinoflagellata (5)
-
miospores
-
pollen (8)
-
-
-
Plantae
-
algae
-
diatoms (1)
-
-
Pteridophyta
-
Filicopsida
-
Azolla (1)
-
-
-
Spermatophyta
-
Angiospermae
-
Dicotyledoneae
-
Alnus (1)
-
Betula (1)
-
Corylus (1)
-
Fagus (1)
-
Juglans (1)
-
Quercus (1)
-
-
Monocotyledoneae
-
Palmae (1)
-
-
-
Gymnospermae
-
Coniferales
-
Pinaceae
-
Pinus (1)
-
-
Taxodiaceae
-
Sequoia (1)
-
-
Taxodium (1)
-
Tsuga (1)
-
-
-
-
-
-
geochronology methods
-
K/Ar (1)
-
paleomagnetism (4)
-
-
geologic age
-
Cenozoic
-
Quaternary
-
Pleistocene
-
lower Pleistocene
-
Gelasian (2)
-
-
Matuyama Chron (1)
-
-
upper Quaternary
-
Brunhes Chron (1)
-
-
-
Tertiary
-
Neogene
-
Miocene
-
lower Miocene
-
Aquitanian (3)
-
Burdigalian (1)
-
-
middle Miocene
-
Langhian (1)
-
Serravallian (1)
-
-
-
Pliocene
-
upper Pliocene (1)
-
-
-
Paleogene
-
Eocene
-
middle Eocene
-
Lutetian (1)
-
-
-
Oligocene
-
lower Oligocene
-
Rupelian (1)
-
-
upper Oligocene
-
Chattian (1)
-
-
-
Paleocene (1)
-
-
-
upper Cenozoic (1)
-
-
Mesozoic
-
Cretaceous
-
Upper Cretaceous (1)
-
-
-
-
igneous rocks
-
igneous rocks
-
plutonic rocks
-
granites (1)
-
-
volcanic rocks
-
pyroclastics
-
tuff (1)
-
-
-
-
-
metamorphic rocks
-
metamorphic rocks
-
schists (1)
-
-
-
minerals
-
carbonates
-
calcite (1)
-
-
oxides
-
hematite (1)
-
hydroxides
-
iron hydroxides (1)
-
-
maghemite (1)
-
magnetite (1)
-
-
-
Primary terms
-
absolute age (1)
-
Asia
-
Buryat Russian Federation
-
Vitim Plateau (1)
-
-
Central Asia
-
Turgay Basin (1)
-
-
Irtysh River (2)
-
Krasnoyarsk Russian Federation (1)
-
Kulunda Steppe (1)
-
Kurgan Russian Federation (1)
-
Novosibirsk Russian Federation (5)
-
Ob-Irtysh Interfluve (1)
-
Omsk Russian Federation (5)
-
Tomsk Russian Federation (2)
-
Tyumen Russian Federation (1)
-
West Siberia
-
Siberian Lowland (2)
-
-
Western Transbaikalia (1)
-
-
carbon
-
C-13/C-12 (2)
-
C-14 (1)
-
-
Cenozoic
-
Quaternary
-
Pleistocene
-
lower Pleistocene
-
Gelasian (2)
-
-
Matuyama Chron (1)
-
-
upper Quaternary
-
Brunhes Chron (1)
-
-
-
Tertiary
-
Neogene
-
Miocene
-
lower Miocene
-
Aquitanian (3)
-
Burdigalian (1)
-
-
middle Miocene
-
Langhian (1)
-
Serravallian (1)
-
-
-
Pliocene
-
upper Pliocene (1)
-
-
-
Paleogene
-
Eocene
-
middle Eocene
-
Lutetian (1)
-
-
-
Oligocene
-
lower Oligocene
-
Rupelian (1)
-
-
upper Oligocene
-
Chattian (1)
-
-
-
Paleocene (1)
-
-
-
upper Cenozoic (1)
-
-
Chordata
-
Vertebrata
-
Tetrapoda
-
Mammalia
-
Theria
-
Eutheria
-
Rodentia
-
Myomorpha
-
Cricetidae
-
Microtus (1)
-
-
-
-
-
-
-
-
-
-
geophysical methods (3)
-
ground water (2)
-
hydrogen
-
D/H (2)
-
-
igneous rocks
-
plutonic rocks
-
granites (1)
-
-
volcanic rocks
-
pyroclastics
-
tuff (1)
-
-
-
-
Invertebrata
-
Mollusca (1)
-
-
isotopes
-
radioactive isotopes
-
C-14 (1)
-
Rn-222 (1)
-
-
stable isotopes
-
C-13/C-12 (2)
-
D/H (2)
-
O-18/O-16 (2)
-
-
-
Mesozoic
-
Cretaceous
-
Upper Cretaceous (1)
-
-
-
metals
-
actinides
-
thorium (1)
-
uranium (1)
-
-
alkaline earth metals
-
radium (1)
-
-
rare earths (1)
-
-
metamorphic rocks
-
schists (1)
-
-
noble gases
-
radon
-
Rn-222 (1)
-
-
-
oxygen
-
dissolved oxygen (1)
-
O-18/O-16 (2)
-
-
paleobotany (2)
-
paleoclimatology (3)
-
paleoecology (1)
-
paleogeography (2)
-
paleomagnetism (4)
-
palynology (3)
-
palynomorphs
-
Dinoflagellata (5)
-
miospores
-
pollen (8)
-
-
-
Plantae
-
algae
-
diatoms (1)
-
-
Pteridophyta
-
Filicopsida
-
Azolla (1)
-
-
-
Spermatophyta
-
Angiospermae
-
Dicotyledoneae
-
Alnus (1)
-
Betula (1)
-
Corylus (1)
-
Fagus (1)
-
Juglans (1)
-
Quercus (1)
-
-
Monocotyledoneae
-
Palmae (1)
-
-
-
Gymnospermae
-
Coniferales
-
Pinaceae
-
Pinus (1)
-
-
Taxodiaceae
-
Sequoia (1)
-
-
Taxodium (1)
-
Tsuga (1)
-
-
-
-
-
plate tectonics (1)
-
sedimentary rocks
-
clastic rocks
-
claystone (1)
-
sandstone (2)
-
siltstone (2)
-
-
coal (2)
-
-
sediments
-
clastic sediments
-
alluvium (3)
-
clay (1)
-
sand (1)
-
-
marine sediments (1)
-
-
soils
-
loam (1)
-
-
springs (2)
-
stratigraphy (5)
-
-
sedimentary rocks
-
sedimentary rocks
-
clastic rocks
-
claystone (1)
-
sandstone (2)
-
siltstone (2)
-
-
coal (2)
-
-
-
sediments
-
sediments
-
clastic sediments
-
alluvium (3)
-
clay (1)
-
sand (1)
-
-
marine sediments (1)
-
-
-
soils
-
soils
-
loam (1)
-
-
GeoRef Categories
Era and Period
Epoch and Age
Date
Availability
1-20 OF 21 RESULTS FOR
Beshcheul' Formation
Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account
Would you like to receive an alert when new items match your search?
Sort by
1
Journal Article
The Paleogene/Neogene boundary in continental deposits of the West Siberian Plain
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 February 2016
Russ. Geol. Geophys. (2016) 57 (2): 303–315.
..., and Serravallian). We consider the distribution of dinocysts of the genus Pseudokomewuia in the stratotype section of the Zhuravka Horizon (Zashchitino Village) and in the section of borehole 13 (Chelyuskintsev Village), which exposes the Turtas, Abrosimovka, and Beshcheul Formations. Similar compositions...
Journal Article
MAGNETOSTRATIGRAPHIC AND PALEOBOTANICAL DESCRIPTION OF THE MIOCENE DEPOSITS IN THE BESHCHEUL HORIZON OF WEST SIBERIA
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 December 1999
Russ. Geol. Geophys. (1999) 40 (12): 1776–1788.
... change, involving the flora (extinction of the forest mesophilic Turgai flora and formation of the forest-steppe post-Turgai flora). Three stages of the development of the Turgai flora – Tagan, Kas’kovka, and Isakovka – have been outlined by paleobotanical data generalized over the Beshcheul Horizon...
Image
The lithological column and magnetostratigraphic section of the Isakovka ex...
in MAGNETOSTRATIGRAPHIC AND PALEOBOTANICAL DESCRIPTION OF THE MIOCENE DEPOSITS IN THE BESHCHEUL HORIZON OF WEST SIBERIA
> Russian Geology and Geophysics
Published: 01 December 1999
– leaf replicas, 12 – lignitized-wood clastics, 13 – plant debris, 14 – water line, 15 – sampling levels, 16 – reverse polarity, 17 – normal polarity; ns – Novaya Stanitsa beds, nil – Nizhnyaya Il’inka beds, gor – Gorskii Log beds, bs – Beshcheul Formation, ab – Abrosimovka Formation, x
Journal Article
Late Cenozoic paleomagnetism of West Siberian Plate
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 April 2007
Russ. Geol. Geophys. (2007) 48 (4): 337–348.
... N 1 N Nizhnyaya Il’inka beds (bottom of Krutaya Gora Formation), silts, sands; Irtysh region near Omsk (Nizhnyaya Il’inka exp.) 355 55 55 5.2 13 N 1 N Beshcheul Frm (Taganka beds), clays, sands; Ob’ region near Tomsk (Kireevskoe exp.) 21.8 45 37 5.4 18 N 1 R Beshcheul Frm...
Journal Article
Paleomagnetism of the Paleogene–Neogene continental sediments of the Om’ basin ( southern West Siberia )
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 July 2014
Russ. Geol. Geophys. (2014) 55 (7): 881–891.
... magnetization (ChRM). The compiled paleomagnetic section, which includes seven regional horizons and same-named formations (Oligocene Atlym, Novomikhailovka, and Zhuravka Formations and Neogene Abrosimovka, Beshcheul, Tavolzhan, and Novaya Stanitsa Formations), was compared with the Cenozoic polarity scale...
Image
Location of the objects under study ( Babin et al., 2015 ). 1 – Evsino Fo...
in Role of the Water–Rock System in the Formation of the Composition of Radon Water of the Tulinskoe Field (Novosibirsk)
> Russian Geology and Geophysics
Published: 06 June 2024
Fig. 1. Location of the objects under study ( Babin et al., 2015 ). 1 – Evsino Formation (N 1 ev); 2 – Beshcheul Formation (N 1 bš); 3 – Zhuravka Formation (₽ 3 žr); 4 – Lagernotov Formation (₽ 3 lt); 5 – Novomikhailovka Formation (₽ 3 nm); 6 – thrust. Barlak granite–leucogranite
Journal Article
Stratigraphic, paleomagnetic, and palynological data on the Paleogene–Neogene continental sediments of southwestern West Siberia
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 April 2011
Russ. Geol. Geophys. (2011) 52 (4): 466–473.
..., they consist of four formations: Abrosimovka, Beshcheul, Tavolzhan, and Novaya Stanitsa. These sediments are widespread on the southern West Siberian Plain. The Lower Neogene–Lower Miocene. The Abrosimovka Formation overlies the Zhuravka Formation (56.6–50 m) with erosion and is made up of lacustrine...
Journal Article
MICROPHYTOFOSSILS AND MAGNETOSTRATIGRAPHY OF UPPER CRETACEOUS AND CENOZOIC DEPOSITS OF THE SOUTHEASTERN WEST SIBERIAN PLAIN
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 April 2003
Russ. Geol. Geophys. (2003) 44 (4): 338–352.
... Siberian Plain [ 2 ], we recognized marine deposits of the Gan’kino, Lyulinvor (BH-15), and Tavda (BH-2, BH-4, BH-10, and BH-15) Formations ( Fig. 3 ). The Paleogene continental deposits include the Atlym, Novomikhailovka, and Zhuravka Formations. The Miocene includes the Abrosimovka, Beshcheul, Tavolzhan...
Journal Article
PALEOCARPOLOGY AND PROBLEMS OF NEOGENE STRATIGRAPHY OF WEST SIBERIA
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 August 2006
Russ. Geol. Geophys. (2006) 47 (8): 963–970.
... of the Kas’kovka floral level [e.g., 4 , 11 ]. Later on, rich and quite typical floras of this level were identified not only in the Kas’kovka Formation per se but also in the lower beds of the Beshcheul’ and Suzun Formations [ 16 ]; in total, they are now known in more than 70 occurrences. The collections...
Journal Article
PALYNOSTRATIGRAPHY OF PALEOGENE AND NEOGENE SEDIMENTS OF THE BARABA-KULUNDA FACIES ZONE OF WEST SIBERIA
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 November 2011
Russ. Geol. Geophys. (2002) 43 (11): 1017–1037.
... is dated late Middle—Upper Eocene (upper Lutetian—Bartonian—Priabonian). We describe eight palynological assemblages from the continental Paleogene and Neogene deposits and substantiate the establishment of the Zhuravka, Abrosimov, Beshcheul’, and Tavolga Formations in the boreholes. Three stages...
Journal Article
MARINE AND CONTINENTAL PALEOGENE AND MIOCENE OF SOUTHERN BARABA FACIES REGION OF WEST SIBERIA: STRATIGRAPHY AND MICROPHYTOFOSSILS
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 January 2005
Russ. Geol. Geophys. (2005) 46 (1): 60–71.
... ]. The age of the deposits is the Lower Miocene. The basalt deposits of the Abrosimovka Formation which are still characterized by the Late Oligocene spore-and-pollen complex are absent from BH-9. The Beshcheul Formation is recognized in the range 124–90 m. The deposits are represented by finely...
Image
Litho- and magnetostratigraphic reference sections of the Beshcheul Horizon...
in MAGNETOSTRATIGRAPHIC AND PALEOBOTANICAL DESCRIPTION OF THE MIOCENE DEPOSITS IN THE BESHCHEUL HORIZON OF WEST SIBERIA
> Russian Geology and Geophysics
Published: 01 December 1999
Fig. 5. Litho- and magnetostratigraphic reference sections of the Beshcheul Horizon. Q – Quaternary deposits; tg – Tagan Formation, kr – Kireevskoe Formation. Designations follow Fig. 2 .
Image
Location of the studied objects (1–16) within the bounds of the Novosibirsk...
Published: 01 December 2022
Fig. 1. Location of the studied objects (1–16) within the bounds of the Novosibirsk urban agglomeration (the underlying geological data after ( Babin et al., 2015 )). Stratigraphic subdivision: 1 , Evsino Formation (N 1 ev); 2 , Beshcheul Formation (N 1 bš); 3 , Zhuravka Formation (₽ 3 zr); 4
Image
Cross-section through BH-2 and BH-4 (see Fig. 1 ). 1 — clays, 2 — sand...
in MICROPHYTOFOSSILS AND MAGNETOSTRATIGRAPHY OF UPPER CRETACEOUS AND CENOZOIC DEPOSITS OF THE SOUTHEASTERN WEST SIBERIAN PLAIN
> Russian Geology and Geophysics
Published: 01 April 2003
Fig. 2. Cross-section through BH-2 and BH-4 (see Fig. 1 ). 1 — clays, 2 — sands, 3 — silts, 4 — lignite, 5 , 6 — loams, 7 — buried soils. Formations: Gan’kino (K 2 gn), Lyulinvor (E 2 ll), Tavda (E 2 tv), Atlym (E 3 at), Novomikhailovka (E 3 nm), Zhuravka (E 3 zr), Abrosimovka (N 1
Journal Article
Paleogene and Neogene stratigraphy and paleotemperature trend of West Siberia ( from palynologic data )
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 July 2011
Russ. Geol. Geophys. (2011) 52 (7): 709–716.
...., Alnus kefersteinii Ung., and Salvinia mediana Nikit. The Abrosimovka Formation is correlated with the sediments of the Aquitanian stage ( Nikitin, 2006 ; Panova, 1971 ). In the late Early–Middle Miocene (21–18 Ma), a new stage of lacustrine–alluvial sedimentation began (Beshcheul Formation...
Journal Article
PALEOCARPOLOGY AND PROBLEMS OF THE PALEOGENE STRATIGRAPHY OF WEST SIBERIA
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 November 2005
Russ. Geol. Geophys. (2005) 46 (11): 1151–1158.
..., including the phases of the formation (early Early Oligocene-Atlym epoch), progressive development (second half of the Early Oligocene and most of the Late Oligocene; Novomikhailovka and Zhuravka—“Lagerny Sad”—epochs), and gradual degradation of rich mesophilic coniferous–broad-leaved forests (late Late...
Journal Article
Biostratigraphy and deposition environments of the Middle-Late Miocene volcanosedimentary section in the Dzhilinda basin, Western Transbaikalia
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 April 2007
Russ. Geol. Geophys. (2007) 48 (4): 361–370.
... assemblage was found in the Miocene deposits of the Khanda depression in the Baikal foredeep in the lower-middle section of the Bayandai Formation. A typical spore-pollen assemblage of the first half of the Middle Miocene is found as the Kozhevnikovo flora in the lower section of the Beshcheul...
Journal Article
ANALYSIS OF FLORA AND CLIMATE IN WEST SIBERIA AT THE EARLY-LATE PLIOCENE AND PLIOCENE-EOPLEISTOCENE BOUNDARIES
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 May 1998
Russ. Geol. Geophys. (1998) 39 (5): 591–603.
... by a gradual change in the composition of flora and plant associations. The flora composition and plant formations at the end of the Early Pliocene (Bitekei time) differ from the modern ones. They indicate a significantly warmer climate, with average annual temperatures being up to 10° higher than they are now...
Journal Article
Role of the Water–Rock System in the Formation of the Composition of Radon Water of the Tulinskoe Field (Novosibirsk)
D.A. Novikov, A.N. Pyryaev, V.P. Sukhorukov, A.A. Maksimova, A.S. Derkachev, A.F. Sukhorukova, F.F. Dultsev, A.V. Chernykh, A.A. Khvashchevskaya, N.A. Medeshova
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 06 June 2024
Russ. Geol. Geophys. (2024)
...Fig. 1. Location of the objects under study ( Babin et al., 2015 ). 1 – Evsino Formation (N 1 ev); 2 – Beshcheul Formation (N 1 bš); 3 – Zhuravka Formation (₽ 3 žr); 4 – Lagernotov Formation (₽ 3 lt); 5 – Novomikhailovka Formation (₽ 3 nm); 6 – thrust. Barlak granite–leucogranite...
Journal Article
Lower–Middle Pleistocene Stratigraphy of the Southern West Siberian Plain: New Data
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 December 2021
Russ. Geol. Geophys. (2021) 62 (12): 1359–1372.
..., and Kulunda formations of different ages, as well as the Yarovoe and Inguyagun sequences ( Volkova et al., 2016 ). Most of these formations and sequences lack stratotype sections and remain poorly constrained as to the stratigraphic position, range, faunas, and relations of specific geological bodies...
1