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Russian Geology and Geophysics

2022 year, number 1

THREE-DIMENSIONAL MODEL OF OIL AND GAS RESERVOIRS BASED ON GAUSSIAN BEAM PROCESSING OF SCATTERED SEISMIC WAVES

V.A. Cheverda1, M.I. Protasov1, V.V. Lisitsa1, G.V. Reshetova2, D.A. Petrov3, A.A. Mel’nik3, V.V. Shilikov3, R.S. Mel'nikov4, V.V. Volyanskaya4
1Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia
2Institute of Computational Mathematics and Mathematical Geophysics, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Lavrentyeva 6, Novosibirsk, 630090, Russia
3OOO RN-KrasnoyarskNIPIneft', ul. Partizana Zhelesnyaka 24v, Krasnoyarsk, 660022, Russia
4NK Rosneft', Sofiiskaya nab. 26/1, Moscow, 117997, Russia
Keywords: Carbonate reservoir, fracturing, faults, numerical modeling of wave fields, scattered-wave energy field, Gaussian beam

Abstract

The efficiency of the development of an oil and gas field is largely determined by the knowledge of its geologic structure. In the recent decade, complex fractured carbonate reservoirs have attracted more and more attention. This paper is concerned with a new technology for constructing 3D images of complex reservoirs, based on Gaussian beam processing of scattered seismic waves. This technology was developed at OOO RN-KrasnoyarskNIPIneft’ in cooperation with the Trofimuk Institute of Petroleum Geology and Geophysics. To test it, a special synthetic model was constructed, which is analogous to one of the licensed objects of PAO NK Rosneft’. For this purpose, a full-scale 3D seismic modeling was performed, which provided us with synthetic wave fields and made it possible to carry out well-controlled numerical experiments for reconstructing the geologic structure of the object of study. One of the distinctive features of the constructed digital model (digital twin) is the presentation of faults not as some ideal slip surfaces but as 3D geologic bodies filled with tectonic breccias. A series of numerical experiments was performed to simulate such breccias, the geometry of these bodies, and the geomechanical processes of fault formation. To select the parameters of the used method of discrete elements, we used the information obtained by geophysical studies in horizontal wells crossing the fault within the geologic prototype of the constructed digital model.