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Scientific and technical journal

«Proceedings of Gubkin University»

ISSN 2073-9028

Tectonics of southwestern part of oil-and-gas-perspective zone radial fault within Sverdlovsk Ring Megastructure as inferred from seismic survey data

UDC: 550.311
DOI: -

Authors:

DANILOVA EVGENIYA A.1,2

1 Bulashevich Institute of Geophysics, Ural Branch of the Russian Academy of Sciences, Yekaterinburg, Russian Federation
2 Zavaritsky Institute of Geology and Geochemistry, Ural Branch of the Russian Academy of Sciences, Yekaterinburg, Russian Federation

Keywords: Sverdlovsk Ring Megastructure, petroleum potential, geological and geophysical studies, seismic surveying, tectonic faults/discontinuities, hydrocarbon fields, Buzuluk depression, Caspian depression, magnetic anomalies, Sladkovsko-Zarechnaya area, Yasnopolyanskaya area, rhombic fault network

Annotation:

The article examines the tectonic structure of the southwestern part of the presumed radial fault of the Sverdlovsk Ring Megastructure and its influence on the localization of oil and gas fields in the region. The fault zone is associated with hydrocarbon deposits in the Devonian graben-like troughs of Bashkortostan, the Manchazh, Orenburg, and Tashla magnetic anomalies, and the Shalkar seismically active zone in Kazakhstan. 2D and 3D common midpoint (CMP) seismic surveys conducted in the Sladkovsko-Zarechnaya and Yasnopolyanskaya areas within the Orenburg Oblast, and the subsequent interpretation of the data, allowed for a detailed characterization of the deep structure and petroleum potential of these areas. Tectonic processes, including neotectonic ones, have significantly influenced the geological structure and petroleum potential of the region. The identified structures are confined to a rhombic fault network, which coincides with the directions of the ring and radial faults of the megastructure. Tectonic disturbances have been identified in the basement rocks, subsalt and suprasalt deposits; however, no faults have been recorded within the salt sequence itself, which is likely due to their “healing”. The identified deformations appear as numerous combinations of horsts and grabens on the seismic time sections, hydrocarbon deposits being confined to flower structures. It is concluded that the northeastern-striking radial fault of the Sverdlovsk Ring Megastructure significantly influences the tectonics and petroleum potential of the study area. However, hydrocarbon fields are more closely associated with its ring faults.

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