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Sedimentation Conditions, Material Composition, and Reconstruction of the Rock Composition of the Feeding Provinces of the Visean Terrigenous Stage of the Bashkir Dome (Based on the Results of the Study of the Borehole Core in the South of the Perm Territory)

A.V. Plyusnin, A.I. Sulima, D.A. Staroselets, E.M. Tomilina, G.A. Isaeva, I.V. Afonin, I.S. Fedotov, E.S. Rabtsevich, D.M. Bobrov, M.S. Sergeev

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DOI https://doi.org/10.18599/grs.2024.1.5

52-70
rus.

open access

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The lithologic-facial, mineralogical, petrographic, and lithogeochemical studies of Visean terrigenous sediments in the borehole section at the Bashkirian arch were carried out to clarify the sources of matter and sedimentation conditions. Terrigenous rocks of the Radayevsky and Bobrikovsky horizons are characterized by predominantly good sorting and pelletization of clastic material. A significant distance from the source of drifting is assumed. Terrigenous rocks of these horizons are sediments of the first and second sedimentation cycles. The rocks of the Tula horizon are characterized by average sorting and pelletization, which indicates the proximity of the drift source to the sedimentation basin. They are rocks of the first sedimentation cycle. The source of clastic material for the Radayevsky and Tula horizons was found to be rocks of acidic composition. For the beaver horizon, the acidic and the main source of drift was established. It is assumed that sedimentation of rocks occurred in coastal-marine conditions on the passive continental margin, with the inflow of clastic material from the inner parts of the East European Platform, due to overwashing of the early accumulated terrigenous rocks of the Devonian and Proterozoic, as well as destruction of the basement ledges, which were activated in the Early Visean time during the manifestation of folding. The presence of basic rocks in the Bobrikovsky horizon may indicate that the material came from the orogen.

 

Bashkirian arch, Radayevsky, Tula, Bobrikovsky, mineralogy, petrogeochemistry, formation conditions, drift source composition, geodynamics

 

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Aleksey V. Plusnin – Cand. Sci. (Geology and Mineralogy), Head Senior Researcher, Tyumen State University
6, Volodarskogo st. 6, Tyumen, 625003, Russian Federation
 
Alexander I. Sulima – Cand. Sci. (Geology and Mineralogy), Department of Regional and Oil and Gas Geology, Perm State National Research University
15, Bukirev st., Perm, 614000, Russian Federation
 
Dmitry A. Staroselets – Postgraduate student, Tyumen State University
6, Volodarskogo st. 6, Tyumen, 625003, Russian Federation
 
Elena M. Tomilina – Senior Lecturer, Department of Mineralogy and Petrography, Perm State National Research University
15, Bukirev st., Perm, 614000, Russian Federation
 
Galina A. Isaeva – Head of the Mineralogical Research Division, Department of Complex Core Research (Kungur), Branch of OOO LUKOIL-Engineering PermNIPIneft in Perm
3A, Permskaya st., Perm, 614000, Russian Federation
 
Igor V. Afonin – Cand. Sci. (Geology and Mineralogy), Senior Researcher, Research Laboratory of Structural Petrology and Minerageny, National Research Tomsk State University
36, Lenin Ave., Tomsk, 634050, Tomsk, Russian Federation
 
Ivan S. Fedotov – Engineer, Mineralogical Research Division, Department of Complex Core Research (Kungur), Branch of OOO LUKOIL-Engineering PermNIPIneft in Perm
3A, Permskaya st., Perm, 614000, Russian Federation
 
Evgenia S. Rabtsevich – Cand. Sci. (Chemistry), Research Engineer, Center for Collective Use “Analytical Center for Geochemistry of Natural Systems” of the Tomsk State University
36, Lenin Ave., Tomsk, 634050, Russian Federation
 
Dmitry M. Bobrov – Graduate student, Perm State National Research University 
15, Bukirev st., Perm, 614990, Russian Federation
 
Mikhail S. Sergeev – Head of the Department of Acceptance, Systematization, Primary Processing and Storage of Core of the Department of Integrated Core Research (Kungur), Branch of OOO LUKOIL-Engineering PermNIPIneft in Perm
3A, Permskaya st., Perm, 614000, Russian Federation

 

For citation:

Plyusnin A.V., Sulima A.I., Staroselets D.A., Tomilina E.M., Isaeva G.A., Afonin I.V., Fedotov I.S., Rabtsevich E.S., Bobrov D.M., Sergeev M.S. (2024). Sedimentation Conditions, Material Composition, and Reconstruction of the Rock Composition of the Feeding Provinces of the Visean Terrigenous Stage of the Bashkir Dome (Based on the Results of the Study of the Borehole Core in the South of the Perm Territory). Georesursy = Georesources, 26(1), pp. 52–70. https://doi.org/10.18599/grs.2024.1.5