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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

V.V. Silantiev, M.F. Validov, D.N. Miftakhutdinova, N.G. Nourgalieva, E.A. Korolev, B.G. Ganiev, A.A. Lutfullin, K.D. Shumatbaev, R.M. Khabipov, V.A. Sudakov, Yu.A. Akhmadullina, K.A. Golod, A.A. Leontev, R.R. Shamsiev, D.A. Nikonorova, S.S. Krikun, M.V. Noykin, E.A. Abdullina

Original article

DOI https://doi.org/10.18599/grs.2023.4.1

3-28
rus.

open access

Under a Creative Commons license

The paper presents new thickness and sandiness maps of the Visean terrigenous strata (Radayevkian and Bobrikian regional stages, Lower Carboniferous) of the South Tatar Arch, constructed using the “Natural Neighbour” spatial interpolation method in ArcGIS Pro software based on the analysis of geophysical survey data for more than 30,000 boreholes.

The interpretation of the maps in combination with the results of sedimentological, ichnotextural and petrophysical core studies, supplemented by the analysis of archival and published materials, provided an opportunity to update the approach to modelling the sedimentation of the terrigenous Lower Carboniferous of the South Tatar Arch. The proposed sedimentation models of terrigenous and coal-bearing sediments take into account the chronostratigraphic data, the karstification of isolated carbonate platforms, the sediment accumulation rates and the ichnotextural characteristics of the sediments. It is concluded that the accumulation and preservation of terrigenous and peat (coal-bearing) sediments differ in duration (0.1 million years vs. 1.5–2 million years) and are consequently associated with transgressive and regressive phases.

The accumulation of terrigenous sediments includes: (a) transgressive eustatic episodes – short-term incursions of a marine basin onto the eroded surface of an isolated carbonate platform, during which silty and sandy, well-sorted bioturbated sediments were accumulated, often with a variety of ichnofossils of marine benthic organisms; (b) the regressive eustatic phase resulted in the predominant erosion of sediments on the arch; whereas sediments in the incisions were largely preserved.

The accumulation of peat (coal-bearing) deposits includes (a) the regressive eustatic phase, during which the vast area of the eastern Volga-Urals region was covered with flourishing vegetation and stable swamp environments were forming in the incisions of the Tournaisian surface; (b) the transgressive phase – the peat was overlaid and buried by transgressive marine silt-sand sediments; then it was compacted and transformed into coal. The alternation of coal-bearing and transgressive intervals indicates the cyclicity of these processes.

The proposed sedimentation models extend the concepts of previous studies and are consistent with the developed maps of thickness and sandiness of the Lower Carboniferous terrigenous sediments, explaining the complex, covering and mosaic distribution of sand bodies over the area, as well as the filling of incisions with sediments of different lithological types.

 

 

sedimentation, terrigenous Carboniferous, Bobrikian regional stage, incisions, Volga-Urals, oil-bearing, reservoir rocks

 

  • Actualised stratigraphic scheme of Lower Carboniferous sediments of the Volga-Ural subregion. Explanatory note, 2023. Eds. N.K. Fortunatova, E.L. Zaytseva, M.A. Bushueva et al. Moscow: VNIGNI Publ, (in press). (In Russ.)
  • Alekseev V.P. (2014). Atlas of subaquatic facies of the Lower Cretaceous sediments of Western Siberia (Khanty-Mansi Autonomous Okrug-Yugra). Ekaterinburg: Ural State Mining University Publ, 284 p. (In Russ.)
  • Aliev M.M., Vissarionova A.Y., Kuznetsov J.I., Semenova E.G., Sjestnova L.P., Travina L.M., Khachatryan R.O., Shelnova A.K., Yarikov G.M. (1975). Carboniferous of the Volga-Urals oil and gas bearing province. Moscow: Nedra Publ, 261 p. (In Russ.)
  • Aretz M., Herbig H.G., Wang X.D., Gradstein F.M., Agterberg F.P., Ogg, J.G. Chapter 23 – The Carboniferous Period. (2020). Geologic Time Scale 2020. Amsterdam: Elsevier, pp. 811–874.
  • Balseiro D., Powell M.G. (2020). Carbonate collapse and the late Paleozoic ice age marine biodiversity crisis. Geology, 48(2), pp. 118–122. https://doi.org/10.1130/G46858.1
  • Blakey R. (2020). Deep Time Maps Inc. https://deeptimemaps.com
  • Buggisch W., Joachimski M.M., Sevastopulo G., Morrow J.R. (2008). Mississippian δ13Ccarb and conodont apatite δ18O records–Their relation to the Late Palaeozoic Glaciation. Palaeogeography, Palaeoclimatology, Palaeoecology, 268(3–4), pp. 273–292. https://doi.org/10.1016/j.palaeo.2008.03.043
  • Croizé D., Renard F., Gratier, J.-P. Chapter 3. (2013). Compaction and Porosity Reduction. Carbonates: A Review of Observations, Theory, and Experiments. Advances in Geophysics, Ed. R Dmowska. Amsterdam: Elsevier, V. 54, pp. 181–238. https://doi.org/10.1016/B978-0-12-380940-7.00003-2
  • Danilova T.E. (2008). Atlas of rocks of the main oil-bearing horizons of the Paleozoic of the Republic of Tatarstan. Terrigenous rocks of Devonian and Lower Carboniferous. Kazan: Pluton Publ, 440 p. (In Russ.)
  • Davydov V.I., Korn D., Schmitz M.D., Gradstein F.M., Hammer, O. (2012). The Carboniferous period. In: Gradstein, F.M., Ogg, J.G., Schmitz, M.D. and Ogg, G.M. (eds). The Geologic Time Scale 2012, V. 2. Elsevier, Amsterdam, pp. 603–651. https://doi.org/10.1016/B978-0-444-59425-9.00023-8
  • Droser M.D., Bottjer D.J. (1986). A semiquantitative field classification of ichnofabric. Journal of Sedimentary Petrology, 56(4), pp. 556–559. https://doi.org/10.1306/212F89C2-2B24-11D7-8648000102C1865D
  • Emiliani C. (1966). Paleotemperature Analysis of Caribbean Cores P6304-8 and P6304-9 and a Generalized Temperature Curve for the past 425,000 Years. The Journal of Geology, 74(2), pp. 109–124. https://doi.org/10.1086/627150
  • Fielding C.R., Frank T.D., Birgenheier L.P., Rygel M.C., Jones A.T., Roberts J. (2008). Stratigraphic imprint of the Late Palaeozoic Ice Age in eastern Australia: a record of alternating glacial and nonglacial climate regime. Journal of the Geological Society, London, 165, pp. 129–140. https://doi.org/10.1144/0016-76492007-036
  • Fikri H.N., Sachsenhofer R.F., Bechtel A., Gross D. (2022). Organic geochemistry and petrography in Miocene coals in the Barito Basin (Tutupan Mine, Indonesia): Evidence for astronomic forcing in kerapah type peats. International Journal of Coal Geology, 256(February), 103997. https://doi.org/10.1016/j.coal.2022.103997
  • Fortunatova N.K., Zaitseva E.L., Bushueva M.A. (2023). Stratigraphy of the Lower Carboniferous of the Volga-Ural subregion (materials for updating the stratigraphic scheme). Ed. by N.K. Fortunatova. Moscow: VNIGNI Publ., 288 p. (In Russ.)
  • Gafurov Sh.Z., Larochkina I.A., Timofeev A.A., Khasanov R.R. (2000). Kama Coal Basin. Coal base of Russia. Vol 1. Coal basins and deposits of the European part of Russia (Northern Caucasus, Eastern Donbass, Moscow Region, Kama basin, Pechora basin, Urals). Moscow: ZAO Geoinformmark Publ., pp. 133–169. (In Russ.)
  • Golonka J. (2002). Plate-tectonic maps of the Phanerozoic. Society for Sedimentary Geology Special Publications, 72, pp. 21–75. https://doi.org/10.2110/pec.02.72.0021
  • Gorozhanina E.N., Gorozhanin V.M., Zagranovskaya D.E., Zakharova O.A. (2019). About the structure of the Kama-Kinel trough system. Proceedings of higher educational establishments. Geology and Exploration, 3, pp. 9–20. (In Russ.) https://doi.org/10.32454/0016-7762-2019-3-9-20
  • Gruzdev D.A. (2021). Late Devonian-Early Carboniferous isolated carbonate platforms of the North of the Urals and Pay-Khoy. Vestnik geonauk, 10(322), pp. 3–15. (In Russ.) https://doi.org/10.19110/geov.2021.10.1
  • Gubareva V.S. (2003). Carboniferous system. Geology of Tatarstan: Stratigraphy and tectonics. Ed. B.V. Burov. Moscow: GEOS, pp. 103–124. (In Russ.)
  • Gulbranson E.L., Montañez I.P., Schmitz M.D., Limarino C.O., Isbell J.L., Marenssi S.A., Crowley J.L. (2010). High-precision U-Pb calibration of Carboniferous glaciation and climate history, Paganzo Group, NW Argentina. GSA Bulletin, 122(9–10), pp. 1480–1498. https://doi.org/10.1130/B30025.1
  • Haq B.U., Schutter S.R. (2008). A chronology of Paleozoic sea-level changes. Science 322 (5898), pp. 64–68. https://doi.org/10.1126/science.1161648
  • Kalvoda J. (2002). Late Devonian-Early Carboniferous Foraminiferal Fauna: Zonations, Evolutionary events, paleobiogeography and tectonic implications. Masaryk University, Brno. Czech Republic, 39 p.
  • Khisamov R.S., Gatiyatullin N.S., Gafurov Sh.Z., Khasanov R.R. (2009). Geology and resources of the Kama coal basin in the territory of the Republic of Tatarstan. Kazan: FEN Publ, 159 p. (In Russ.)
  • Khisamov R.S., Gubaydullin A.A., Bazarevskaya V.G., Yudintsev E.A. (2010). Geology of carbonate complexly constructed reservoirs of the Devonian and Carboniferous of Tatarstan. Kazan: FEN Publ, 283 p. (In Russ.)
  • Knaust D. (2017). Atlas of Trace Fossils in Well Core: Appearance, Taxonomy and Interpretation. Springer, Switzerland, 209 p. https://doi.org/10.1007/978-3-319-49837-9
  • Kukal Z. (1971). Geology of Recent sediments. London: Academic Press, 490 p.
  • Larochkina I.A. (2005). Principles of subdivision, identification and correlation of the terrigenous Lower Carboniferous sequences. Georesursy = Georesources, 2(17), pp. 15–19. (In Russ.)
  • Larochkina I.A. (2008). Geological bases of prospecting and exploration of oil and gas fields in the Republic of Tatarstan. Kazan: LLC PF Gart Publ, 210 p. (In Russ.)
  • Larochkina I.A., Melnikov S.N. (1984). Palaeogeomorphology of south-eastern Tatarstan in the Early Carboniferous. Geomorfologiya = Geomorphology, 3, pp. 65–69. (In Russ.)
  • Larochkina I.A., Ganiev R.R., Mikhaylova E.N., Novikova I.P. (2010). Influence of erosion and karst incisions on the location of oil deposits in the Radaevkian-Bobrikovian sediments. Georesursy = Georesources, 3(35), pp. 38–41. (In Russ.)
  • Larochkina I.A., Mikhaylova E.N., Novikov I.P. (2011). Bobrikov partial barriersas objects of highly effective exploitation of deposit (on example of Ulyanovsk deposit). Georesursy = Georesources, 4(40), pp. 27–30. (In Russ.)
  • Makhlina M.H.,. Vdovenko M.V., Alekseev A.S., Byvsheva T.V., Donakova L.M., Zhulitova V.E., Kononova L.I., Umnova N.I., Shik E.M. (1993). The Lower Carboniferous of the Moscow Syneclise and Voronezh Anteclise. Moscow: Nauka, 221 p. (In Russ.)
  • Mii H.-S., Grossman E.L., Yancey T.E., Chuvashov B., Egorov A. (2001). Isotopic records of brachiopod shells from the Russian Platform: Evidence for the onset of Mid-Carboniferous glaciation. Chemical Geology, 175, p. 133147. https://doi.org/10.1016/S0009-2541(00)00366-1
  • Mikulash R., Dronov A.V. (2006). Paleoichnology – an introduction to the study of fossil traces of vital activity. Prague: Geological Institute of the Academy of Sciences of the Czech Republic, 122 p. (In Russ.)
  • Moore T.A., Shearer J.C. (2003). Peat/coal type and depositional environment – Are they related? International Journal of Coal Geology, 56(3–4), pp. 233–252. https://doi.org/10.1016/S0166-5162(03)00114-9
  • Muslimov R.Kh., ed. (2007). Oil and gas resources of the Republic of Tatarstan. Geology and development of oil fields. Vol. 1. Kazan: Fen Publ, 316 p. (In Russ.)
  • Muslimov R.Kh., Vasyasin G.I., Shakirov A.N., Chendarev V.V. (1999). Geology of the Tournaisian Stage of Tatarstan. Kazan: Monitoring Publ, 186 p. (In Russ.)
  • Nikishin A.M., Ziegler P.A., Stephenson R.A., Cloetingh S.A.P.L., Furne A.V., Fokin P.A. et al. (1996). Late Precambrian to Triassic history of the East European Craton: Dynamics of sedimentary basin evolution. Tectonophysics, 268(1–4), pp. 23–63. https://doi.org/10.1016/S0040-1951(96)00228-4
  • Pozner V.M. (1975). Carboniferous period. Palaeogeography. Palaeogeography of the USSR. Explanatory note to the Atlas of the Lithological and Palaeogeographic Maps of the USSR. Vol. 2. Devonian, Carboniferous, Permian. Moscow: Nedra Publ, pp. 62–119. (In Russ.)
  • Pozner V.M., Kirina T.I., Porfiriev G.S. (1957). Volga-Ural oil-bearing province. Carboniferous deposits. Proceedings of the All-Union Petroleum Research Geological Exploration Institute, 112. Leningrad: Gostoptekhizdat Publ, 312 p. (In Russ.)
  • Saltzman M.R. (2003). Late Paleozoic ice age: Oceanic gateway or pCO2? Geology 31, pp. 151–154. https://doi.org/10.1130/0091-7613(2003)031<0151:LPIAOG>2.0.CO;2
  • Scotese C. R. (2010). PALEOMAP Project. http://www.scotese.com/earth.htm
  • Seilacher A. (1964). Sedimentological classification and nomenclature of trace fossils. Sedimentology, 3, pp. 256–263.
  • Seilacher A. (1967). Bathymetry of trace fossils. Marine Geology, 5(5–6), pp. 413–428. https://doi.org/10.1016/0025-3227(67)90051-5
  • Shelnova A.K., Zheltova A.N., Bludorova E.A. (1966). Types of the Lower Carboniferous sections developed in the Tatar ASSR. Doklady Akademii Nauk USSR, 171(2), pp. 435–438. (In Russ.)
  • Shinn E.A., Robbin D.M. (1983). Mechanical and chemical compaction in fine-grained shallow-water limestones. Journal of Sedimentary Petrology, 53(2), pp. 595–618. https://doi.org/10.1306/212F8242-2B24-11D7-8648000102C1865D
  • Sibson R. (1981). A brief description of natural neighbor interpolation (Ch. 2). Interpreting Multivariate Data. Chichester: John Wiley, pp. 21–36.
  • Silantiev V.V., Validov M.F., Miftakhutdinova D.N., Morozov V.P., Ganiev B.G., Lutfullin A.A., Shumatbaev K.D., Khabipov R.M., Nurgalieva N.G., Tolokonnikova Z.A., Korolev E.A., Sudakov V.A., Smirnova A.V., Golod K.A., Leontiev A.A., Shamsiev R.R., Noykin M.V., Kosarev V.E., Nikonorova D.A., Akhmetov R.F. (2022). Sedimentation model of the middle Devonian clastic succession of the South Tatar Arch, Pashyian Regional stage, Volga-Ural Oil and Gas Province, Russia. Georesursy = Georesources, 24(4), pp. 12–39. (In Russ.) https://doi.org/10.18599/grs.2022.4.2
  • Silantiev V.V., Gutak Ya.M., Tichomirowa M., Kulikova A.V., Felker A.S., Urazaeva M.N., Porokhovnichenko L.G., Karasev E.V., Bakaev A.S., Zharinova V.V., Naumcheva M.A. (2023). First radiometric dating of tonsteins from coal-bearing succession of the Kuznetsk Basin: U-Pb geochronology of the Tailugan Formation. Georesursy = Georesources, 25(2), pp. 203–227. https://doi.org/10.18599/grs.2023.2.15
  • Smelkov V.M., Tukhvatullin R.K., Uspensky B.V. (2007). Oil and gas resources of the Paleozoic reservoirs of Tatarstan. Oil and gas resources of the Republic of Tatarstan. Geology and development of oil fields. Vol. 1. Ed. R.Kh. Muslimov. Kazan: Fen Publ, pp. 52–65. (In Russ.)
  • Torsvik T.H., Cocks L.R.M. (2017). Earth History and Palaeogeography. Cambridge University Press, Cambridge, UK. https://doi.org/10.1017/9781316225523
  • Troepolskiy V.I., Badamshin E.Z., Tukhvatullin R.K. (1974). Patterns of oil-bearing development and prospecting techniques in the Kama-Kinel trough system in the territory of Tatarstan. Problems of geology and oil resources of the Middle Volga region, 4. Kazan: Kazan University Publ., pp. 3–28. (In Russ.)
  • Van Hengstum P.J., Maale G., Donnelly J.P., Albury N.A., Onac B.P., Sullivan R.M., Winkler T.S., Tamalavage A.E., MacDonald D. (2018). Drought in the northern Bahamas from 3300 to 2500 years ago. Quaternary Science Reviews, 186, pp. 169–185. https://doi.org/10.1016/j.quascirev.2018.02.014
  • Wright V.P., Vanstone S.D. (2001). Onset of Late Palaeozoic glacio-eustasy and the evolving climates of low latitude areas: a synthesis of current understanding. Journal of the Geological Society, 276, pp. 579–582. https://doi.org/10.1144/jgs.158.4.579
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Vladimir V. Silantiev – Dr. Sci. (Geology and Mineralogy), Head of Department of Paleontology and Stratigraphy, Institute of Geology and Petroleum Technology, Kazan Federal University
18 Kremlevskaya st., Kazan, 420008, Russian Federation
e-mail: Vladimir.Silantiev@kpfu.ru

Marat F. Validov – Lead Engineer, Head of Petrophysical Department, Center for Excellence of Digital Technologies in the Oil and Gas Industry, Institute of Geology and Petroleum Technology, Kazan Federal University
18 Kremlevskaya st., Kazan, 420008, Russian Federation

Dinara N. Miftakhutdinova – Assistant of Department of Paleontology and Stratigraphy, Kazan Federal University
18 Kremlevskaya st., Kazan, 420008, Russian Federation

Nouria G. Nourgalieva – Dr. Sci. (Geology and Mineralogy), Professor, Department of Oil and Gas Geology named after Academician A.A. Trofimuk, Institute of Geology and Petroleum Technology, Kazan Federal University
18 Kremlevskaya st., Kazan, 420008, Russian Federation

Eduard A. Korolev – Cand. Sci. (Geology and Mineralogy), Head of Department of General Geology and Hydrogeology, Institute of Geology and Petroleum Technology, Kazan Federal University
18 Kremlevskaya st., Kazan, 420008, Russian Federation

Bulat G. Ganiev – Head of the Department of Field Development, Tatneft PJSC
75 Lenin st., Almetyevsk, 423450, Russian Federation

Azat A. Lutfullin – Deputy Head of the Department of Field Development, Tatneft PJSC
75 Lenin st., Almetyevsk, 423450, Russian Federation

Kirill D. Shumatbaev – Chief Expert (on petrophysical research), Department of Field Development, Tatneft PJSC
75 Lenin st., Almetyevsk, 423450, Russian Federation

Rishat M. Khabipov – Head of the Field Development and Subsoil Use Monitoring Division, Department of Field Development, Tatneft PJSC
75 Lenin st., Almetyevsk, 423450, Russian Federation

Vladislav A. Sudakov – Deputy Director of the Institute for Innovation, Center for Excellence of Digital Technologies in the Oil and Gas Industry, Institute of Geology and Petroleum Technology, Kazan Federal University
18 Kremlevskaya st., Kazan, 420008, Russian Federation

Yuliya A. Akhmadullina – Engineer, Center for Excellence of Digital Technologies in the Oil and Gas Industry, Institute of Geology and Petroleum Technology, Kazan Federal University
18 Kremlevskaya st., Kazan, 420008, Russian Federation

Kseniya A. Golod – Engineer, Center for Excellence of Digital Technologies in the Oil and Gas Industry, Institute of Geology and Petroleum Technology, Kazan Federal University
18 Kremlevskaya st., Kazan, 420008, Russian Federation

Aleksey A. Leontev – Lead Engineer, Head of Well Logging Interpretation Department, Center for Excellence of Digital Technologies in the Oil and Gas Industry, Institute of Geology and Petroleum Technology, Kazan Federal University
18 Kremlevskaya st., Kazan, 420008, Russian Federation

Ruslan R. Shamsiev – Engineer, Center for Excellence of Digital Technologies in the Oil and Gas Industry, Institute of Geology and Petroleum Technology, Kazan Federal University
18 Kremlevskaya st., Kazan, 420008, Russian Federation

Daria A. Nikonorova – Assistant, Center for Excellence of Digital Technologies in the Oil and Gas Industry, Institute of Geology and Petroleum Technology, Kazan Federal University
18 Kremlevskaya st., Kazan, 420008, Russian Federation

Svetlana S. Krikun – Assistant, Center for Excellence of Digital Technologies in the Oil and Gas Industry, Institute of Geology and Petroleum Technology, Kazan Federal University
18 Kremlevskaya st., Kazan, 420008, Russian Federation

Mikhail V. Noykin – Engineer, Center for Excellence of Digital Technologies in the Oil and Gas Industry, Institute of Geology and Petroleum Technology, Kazan Federal University
18 Kremlevskaya st., Kazan, 420008, Russian Federation

Elina A. Abdullina – Engineer, Center for Excellence of Digital Technologies in the Oil and Gas Industry, Institute of Geology and Petroleum Technology, Kazan Federal University
18 Kremlevskaya st., Kazan, 420008, Russian Federation

 

For citation:

Silantiev V.V., Validov M.F., Miftakhutdinova D.N., Nourgalieva N.G., Korolev E.A., Ganiev B.G., Lutfullin A.A., Shumatbaev K.D., Khabipov R.M., Sudakov V.A., Akhmadullina Yu.A., Golod K.A., Leontev A.A., Shamsiev R.R., Nikonorova D.A., Krikun S.S., Noykin M.V., Abdullina E.A. (2023). 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 = Georesources, 25(4), pp. 3–28. https://doi.org/10.18599/grs.2023.4.1