PSI - Issue 6

A. Sidelnik / Procedia Structural Integrity 6 (2017) 316–321

321

Sidelnik Angelina// Structural Integrity Procedia 00 (2017) 000 – 000

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Figure 6. Comparison of the calculation results with the RGB coherence cube (A)

Conclusion Thus, applying the method of stress inversion, we have the opportunity to build a map of the fault tectonics of the region, as well as to determine the most probable direction of the tectonic driver. This allows us to determine the characteristics of the fault, take into account the heterogeneity in the stress field, form recommendations for drilling and hydraulic fracturing. References 1. Lukin S.V., Zhigulskiy S.V., Ovcharenko Yu.V., Challenges for high - performance computing, Oil&Gas Joirnal, 2017, № 5, p. 38 - 42. 2. Maerten L., Maerten F., Lejri M., Gillespie P. Geomechanical paleosress inversion using fracture data // Journal of Structural Geology. 2016. № 89. p. 197-213. 3. Ovcharenko Yu.V., Lukin S.V., Tatur O.A., Kalinin o.Yu., Kolesnikov D.S., Esipov S.V., Zhukov V.V., Demin V.Yu., Volokitin Ya., Sedned A., Podberezhnyy M., Experience in 3D geomechanichal modeling, based on one of the West Siberia oilfield (In Russ.), SPE 182031, 2016 4. Terzaghi, K. 1943. Theoretical Soil Mechanics, John Wiley and Sons, NewYork. 5. Zoback M.D., 2007. Reservoir Geomechanics: Earth Stress and Rock Mechanics Applied to Exploration, Production and Wellbore Stability - Cambridge Press – P. 449.