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Stavropol Arch

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Journal Article
Published: 01 June 2023
Russ. Geol. Geophys. (2023) 64 (6): 743–754.
...V.V. Belyavsky Abstract —Interpretation of magnetotelluric data within the North Caucasus marginal massif, the uplift of the Main Range, and the Stavropol Arch, performed on the basis of one- and two-dimensional inversions of the impedance tensor components and three-dimensional mathematical...
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Image
Arrangement of the MTS profiles on the map of the structural zoning of the ...
Published: 01 June 2023
trough, 3 – East Kuban trough, 4 – Stavropol arch, 5 – Terek–Kuma depression, 6 – Terek–Caspian through; the Greater Caucasus fold system: 7 – North Caucasian marginal massif, 8 – Mineralnye Vody ledge, 9 – Front Range, 10 – Main Range, 11 – Paleozoic ledges, 12 – Mesozoic folded formations; 2
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1972
AAPG Bulletin (1972) 56 (9): 1711–1722.
... such as the Stavropolarch and the Yeysk-Berezan zone of uplifts, where the Lower Cretaceous and Paleogene are productive. In 1971 almost 35.8 million tons of oil and more than 27.7 billion cu m of gas were produced. Exploration and development in 1971 in the eastern part of the district (Daghestan ASSR...
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Journal Article
Published: 01 January 2024
Russ. Geol. Geophys. (2024) 65 (1): 5–19.
... of oil, were discovered in the Volga–Ural OGP on the territory of the South Tatar arch and the Buzuluk Depression. In the Republic of Bashkortostan, industrial oil inflows of up to 50 m 3 /day from the middle upper Frasnian deposits were found in 12 fields ( Varlamov et al., 2020 ). In the Timan...
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Journal Article
Published: 01 April 2009
Russ. Geol. Geophys. (2009) 50 (4): 320–326.
... of sedimentation basins, during subhorizontal microdislocations measured via Poisson’s ratio and Protod’yakonov “arch”. This effect can be reached on hydrofracturing. A possibility of fluid hydrocarbon migration beyond the modern-day oil and gas pools is discussed, thus demonstrating that there are no traces...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1973
AAPG Bulletin (1973) 57 (2): 235–243.
... Barents arch where prospects are poor. Farther east, the Kara Sea is an offshore continuation of the rich West Siberian basin. East of Severnaya Zemlya, the Laptev Sea appears to be most prospective in its western end, close to the Khatanga trough. Upper Paleozoic and Mesozoic rocks are prospective...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1927
AAPG Bulletin (1927) 11 (5): 493–513.
... abruptly on the south by a zone of transverse faults and flexures which trends generally east-northeast to west-southwest. In the southern part of the central Russian Basin are two anticlines trending northeast-southwest: the Trans-Volga Anticline, a flat arch of Upper Carboniferous and Permian beds...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1934
AAPG Bulletin (1934) 18 (5): 603–671.
... to this viewpoint, the general tectonic structure of the Caucasus appears as follows: north and south of the main Caucasian Range are two hard plates, (1) the pre-Caucasian, consisting of the Stavropol plate with two deep depressions, the pre-Kuban and pre-Terek, and (2) the trans-Caucasian, divided by the Suram...
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—USSR continental-shelf tectonic nomenclature: *  (1) Precambrian platform;...
Published: 01 February 1973
; VI —Central Karakum dome; VII —Promyslovka-Buzachi zone of elevations; VIII —Kara-Bogaz dome; IX —Manych channel; X —Stavropol’ dome; Xl —Bolshoy (Great) Caucasus mega-antichnorium; XII —megaanticlinorium in Malyy (Lesser) Caucasus; XIII -Rioni depression; XIV —Kura depression: XV —South
Image
—USSR continental-shelf tectonic nomenclature: *  (1) Precambrian platform;...
Published: 01 February 1973
; VI —Central Karakum dome; VII —Promyslovka-Buzachi zone of elevations; VIII —Kara-Bogaz dome; IX —Manych channel; X —Stavropol’ dome; Xl —Bolshoy (Great) Caucasus mega-antichnorium; XII —megaanticlinorium in Malyy (Lesser) Caucasus; XIII -Rioni depression; XIV —Kura depression: XV —South
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1986
AAPG Bulletin (1986) 70 (10): 1566–1577.
... in the Frolov region and an oil pool in South Kharampur field in the Middle Ob region. Oil yields are usually low. Only 1 well out of 7 yields more than 65 BOPD. An active exploration campaign for oil in the Tyumen Formation continued on the regional Krasnoleninsk arch in the Frolov region ( Figure 1...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1963
AAPG Bulletin (1963) 47 (7): 1294–1347.
...-inch and a 32-inch line from Stavropol, and by lines from the Shebelinka field in the Ukraine and from fields of the Carpathian foreland. The outstanding exploration event of 1962 was the finding of oil in the Lower Cambrian in a well which blew out on March 18 at Markovo on the bank of the Lena...
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Series: AAPG Memoir
Published: 01 January 2012
DOI: 10.1306/13291384M953444
EISBN: 9781629810096
... Cenozoic and has its own distinct tectonic history ( Glumov et al., 2004 ). The South Caspian Basin began as part of a marginal sea ( Zonenshein and Le Pichon, 1986 ). Neotethys closed in the late Tertiary, and the Caucasus Mountains and Stavropol Arch formed, diverting the Volga River from the Black Sea...
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Series: AAPG Memoir
Published: 01 January 2005
DOI: 10.1306/1061783M863175
EISBN: 9781629810430
... 16,598 17,925 34,522 21,925 39,850 56,447 61 6 20300102 Tertiary Reservoirs Oil 47,285 62,025 109,310 19,605 81,630 128,914 85 7 20210101 Central Arch Horst-Block Anticlinal Oil and Gas Oil 84 6142 6226 19,190 25,331 25.416 24 8 71920102 Akata Reservoirs Oil 0 0 0...
Series: AAPG Memoir
Published: 01 January 2003
DOI: 10.1306/M78834C2
EISBN: 9781629810539
... ) and in strike-slip zones ( Christie-Blick and Biddle, 1985 ). There are two ideas for the early formation of rifts. Falvey (1974) proposed that rifts form as crestal normal faults above a rising arch, and therefore, the initiation of arching must precede basin formation. Harding (1984) notes...
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Series: Geological Society, London, Memoirs
Published: 01 January 2006
DOI: 10.1144/GSL.MEM.2006.032.01.29
EISBN: 9781862394070
... extensional provinces and basin development may have occurred in the Devonian in the Peace River Arch area (pericratonic, oblique to the margin of the CC; see Stephenson et al . 1989 ) and in Hudson Bay (intracratonic, reportedly Early-mid-Devonian, not Late Devonian; Hanne et al . 2004 ) and were...
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