About the structure of the Kama-Kinel trough system-Reference-Cited by-同舟云学术

About the structure of the Kama-Kinel trough system

Published:2019-06-28 Issue:3 Volume: Page:9-20
ISSN:2618-8708
Container-title:Proceedings of higher educational establishments. Geology and Exploration
language:
Short-container-title:Izvestiya Vysshikh Uchebnykh Zavedeniy. Geologiya i Razvedka

Author:

Gorozhanina E. N.¹,Gorozhanin V. M.¹,Zagranovskaya D. E.²,Zakharova O. A.²

Affiliation:

1. Institute of Geology — Subdivision of the Ufa Federal Research Centre of the Russian Academy of Sciences (IG UFRC RAS)

2. Gazpromneft Science & Technology Centre

Abstract

Kama-Kinel Trough System (KKTS) — the structure formed in the Frasnian of the Late Devonian in the vast territory of the Volga-Ural province, is distinguished by the Upper Devonian — Lower Carboniferous deposits. The new interpretation of forming conditions of carbonate deposits in the KKTS has been given. The troughs of the KKST were formed in the Late Devonian as basin with gently sloping shelf zones. The deposits of the middle shelf (ramp), gently sinking into the side of the pool, where the layered accumulated precipitation are presented by bioclastic and intraclastic (lumpy) limestones and carbonate breccia, formed under the influence of storms. Three structural-facial zones, central, border and arched, allocated in the structure of deflections of the KKTS, reflect the structure of troughs formed as a result of tectonic restructuring at the beginning of the Visean and reactivated at the neotectonic stage. The uplift of the side zone considered as the reef buildups seem to be horst-shaped structures in fault zones. These features allow us to consider the structure of the KKTS as formed as a result of paleotectonic processes with the appropriate distribution of shallow and deep-water facies, subsequently changed as a result of reactivation of the basement faults.

Publisher

Sergo Ordshonikidze University

Subject

General Chemical Engineering

Reference21 articles.

1. Antoshkina A.I. Rifoobrazovanie v paleozoe (sever Urala i sopredel’nye oblasti). [A reef-formation during Paleozoic (the north of the Urals and neighbor regions)], Ekaterinburg, UrO RAN Publ., 2003, 303 p. (In Russian).

2. Valeev R.N. Gorizontal’nye sdvigovye dvizhenija zemnoj kory vostoka Russkoj platformy. [The horizontal strike-sleep motions of the earth crust at the east of the Russian Platform] Novye dannye po geologii i neftenosnosti Volgo-Kamskogo kraja. [New data on the geology and oil-bearing of the Volga-Kama region] Trudy Geologicheskogo instituta (g. Kazan) [Proc. of the Geological Institute (Kazan city)], Kazan, Kazan Publ., 1970, no. 30, pp. 90–98. (In Russian).

3. Geologija i neftegazonosnost’ Kamsko-Kinel’skih progibov [Geology and oil-gas- bearing of the Kama-Kinel thrughs]. Trudy soveshhanija, Kazan’, sentjabr’, 1969. Red.: V.I.Troepol’skij [Proc. of the conference, Kazan, September 1969, ed. V.L. Troepolsky], Kazan, Kazan University Publ., 1970, 307 p. (In Russian)

4. Grachevsky M.M. Stratigraficheskie i paleogeograficheskie predposylki poiskov novyh zalezhej nefti v Kamsko-Kinel’skoj vpadine [Stratigraphic and paleogeographic preconditions of new oil pools searching in the Kama-Kinel thrugh]. Geologija i neftegazonosnost’ jugo-vostoka Russkoj platformy. Red. R.B.Sejful’-Muljukov [Geology and oil-gas-bearing at the south east of the Russian Platform. Ed. R.B. Sejful-Muljukov] Leningrad, Gos. nauch.-teh. izd-vo neft. i gorno-topl. lit-ry, 1963 (Trudy NILNEFTEGAZ, vyp. 10) [Trudy NILNEFTEGAZ, no. 10], Leningrad, Gostoptechizgat Publ., 1963, pp.79–97. (In Russian)

5. Gutman I.S., Potemkin G.N., Volk E.Ju., Papuhin S.P. Osobennosti geologicheskogo stroenija nizhnekamennougol’nyh otlozhenij v predelah juzhnoj chasti KamskoKinel’skoj sistemy progibov [The peculiarities of the geological structure of the Lower Carboniferous deposits in the limits of the southern part of the Kama-Kinel trough system] Nedropol’zovanie XXI vek [Mineral resources development XXI century], 2011, no5, pp. 20–25. (In Russian)

Cited by 5 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Technique and results of determination of vertical variations in rock thermal properties, temperature gradient and heat flow;Geothermics;2024-01

2. Visean terrigenous sediments of the South Tatar Arch (Volga-Urals oil and gas bearing province) – multifacial filling of the karst surface of the Tournaisian isolated carbonate platform;Georesursy;2023-12-30

3. Biostratigraphy and lithofacies of the Middle-Upper Devonian in the Ayazovo oil field (North-Eastern of Bashkiria);LITHOSPHERE (Russia);2023-03-01

4. Geological prerequisites for the search for rocks with increased reservoir properties in domanic type sediments on the territory of the Republic of Tatarstan;Georesursy;2022-12-20

5. INTERREGIONAL CORRELATION OF THE MIDDLE FRASNIAN (UPPER DEVONOIAN) OF THE NORTH-WEST OF THE RUSSIAN PLATE AND THE EAST OF THE PECHORA PLATE: AN ECOGEOCHEMICAL ASPECT;Geodynamics & Tectonophysics;2022-04-18