Multi-Scaled Structural Spatio-Temporal Analytics for the Evolution of Geology According to A. Einstein Formula
DOI:
https://doi.org/10.9734/bpi/castr/v15/12222DKeywords:
Energy, material, structure, evolution, cognitive geologyAbstract
The authors present the scientific grounding of a new theoretical concept of geo-exploration work, of geo-physical and geo-mechnical models for the unconventional technically recoverable hydrocarbon reserves of the Cis-Ural region. The paper describes heterogeneous balanced volumetric geo-mechanical model for the structural massif of mountain rock post-sedimentation in view of geo-physical synergy and petro-migration. The paper also provides a set of additional studies for seismic, tectono-physical, geological, geo-physical information in a process of search and exploration of hydrocarbon fields and large-scaled construction of surface and subsurface equipment, well drilling and their completion, as well as geo-dynamic studies, geo-hydrogeological simulation of their development stages. The authors have studied the change in stress-deformed status of mountain massifs and the wells in a process of their subsurface operation. They also hae studied the stress fields for the large-scaled reef formations in Zhiguli dislocation and the Cis-Ural region. The authors have scientifically proved the inertia-capillary law of movement conservation (by Darcy-Stokes) and stress-deformed status of square compaction and structural packs of geo-physical rhythms during filtration, petro-migration diffusion and mass-transfer (Bessel’s ray-path and Gaussian distribution). Basing upon the solution of equations related to number of movements (of Navier-Stokes type) for the deformed porous media and conjugated seismic emission of various mass transfer structures the group of authors in a form of a system, have combined filtration as per Darcy and diffusion of structural-topological dislocation of impulses as per Euler with mobile neo-tectonics in porous-cavernous-fractured dissipative accumulation of spectral-phase sedimentation and accumulation of hydrocarbons.