[0005] (1) The existing multi-point geostatistical modeling algorithms are all based on grid pixels, and the training images represent the
spatial distribution pattern of geological bodies in the form of a three-dimensional grid model, which can simulate the space between multiple grids The positional relationship is very beneficial in characterizing the
spatial distribution of complex sedimentary
facies types. Generally, it is only used to characterize the matrix part of fractured reservoirs, and the traditional discrete fracture modeling method is still used for the fracture part, such as the literature "Fracture-cavity
carbonate Modeling of rock reservoirs and research on remaining
oil distribution" (Li Hongkai et al., China University of Geosciences (Beijing) 2012.6), the
matrix model was established using multi-point geostatistics, and the fracture model was established in three directions using traditional discrete fracture modeling , the multi-point geostatistical method was not used in the fracture model; in the literature "Research on
karst facies-controlled modeling methods in weathered
karst areas of
carbonate rocks" (Xinjiang
Petroleum Geology, 2015.6), multi-point geostatistics was used to establish the
karst facies model , using a
deterministic method to build large-scale fractures, using random discrete fracture modeling to build a fracture model, and did not use the multi-point geostatistical method in the fracture model
[0006] (2) In terms of the discrete fracture modeling
algorithm, the predecessors only improved some links in the
simulation framework. The
simulation method first generates the fracture development value according to the fracture
density field, and then generates the fracture occurrence according to the statistical fracture occurrence. Fractures are generated artificially given the fracture shape, such as in the literature "Stochastic Modeling Method for Discrete Fracture Networks" (Zheng Songqing et al., "Journal of
Petroleum and
Natural Gas", Vol. 31, No. 4, pp. 106-110, August 2009) , use the spatial variable probability method to determine the fracture location, use the circular statistical method to analyze the fracture occurrence, and use the Fisher distribution and fractal distribution to simulate the fracture occurrence and geometric parameters. It is necessary to give the location probability and fracture geometric parameters for different series of fractures. , the distribution of existing fractures cannot be considered in the simulation process, but this method cannot reflect the
spatial configuration of discrete fractures; in the literature "Using seismic data to constrain the spatial distribution of small-scale discrete The
density model is transformed into a
probability model, and the
probability model is used as the termination condition of the simulation to solve the matching problem between the simulated fracture density and the well
point data, and this method cannot solve the problem of three-dimensional space configuration of multi-series fractures
[0007] (3) Scholars have tried to apply the idea of multi-point geostatistics to fracture modeling, and the simulation results can reflect the complex spatial configuration of fractures. In Acta Sinica, 2017.6), multi-point geostatistics is used to establish a fracture model, which can consider the spatial configuration relationship of fractures, but the fractures are represented by a grid method, which cannot simulate fractures with a grid scale similar to or smaller than the grid scale. Unable to accurately characterize crack density
[0008] Therefore, the current technical status in this field is: multi-point geostatistical modeling is usually used to simulate 3D geological bodies with equal volumes of sediments in matrix properties; discrete fracture modeling methods only use parameters such as fracture density, occurrence, and shape The statistical law of each group of fractures is simulated separately, and the spatial configuration relationship of multi-scale fractures and multi-series fractures cannot be considered; in the prior art, the pixel grid is used to represent the spatial distribution of fractures, and the existing multi-point geostatistical method is used. Establishing a fracture model, using a pixel grid to represent discrete fractures limits the parameters such as the scale and opening of the fracture, which will result in the inability to simulate fractures smaller than the grid scale and the approximate size of the grid scale, and it is also impossible to simulate multi-scale fractures, which seriously affects the Accuracy of fracture simulation