Intelligent inversion method for far-field stress state
A stress state and far-field technology, applied in the field of geological stress field simulation, can solve the problems of cumbersome efficiency and manual intervention
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Embodiment 1
[0041] Such as figure 1 As shown, the intelligent inversion method of the far-field stress state described in the present invention is suitable for the unknown far-field stress state. On the basis of the existing geological model, through cyclical trials, the efficient method for finally determining the far-field stress state that meets the actual geological conditions A fast and intelligent method belongs to the technical field of geological stress field simulation. The present invention comprises the steps:
[0042] S1: Construction of 3D geological model: Select the region where the far-field stress state is unknown and some constraint points are known as the geological region to be constructed, and use the 3D modeling software to establish a geological region that conforms to the actual reservoir geology based on the geological structure map of the geological region. 3D geological model to reflect the spatial distribution characteristics of the undulations of the actual f...
Embodiment 2
[0071] Assuming that the study area with unknown far-field stress state is located in the Zhanhua Sag belonging to the Jiyang Depression in the Bonan Sag, it is a third-order structural unit of the Zhanhua Sag, and the north is controlled by the Chengnan fault zone and the Chengdong Uplift , connected with Chenjiazhuang in the south, controlled by the Guxi fault, Gubei depression and Gudao bulge in the east, and connected in the southeast by the Kenxi horst, Sanhezhuang depression and Guxi depression. Such as figure 2 As shown, the Bonan subsag is a broom-shaped fault that is high in the north and low in the south, and is clamped by two basin-dip syngeneic faults and the Guxi fault. Block Yi 176 is located in the Yi 176-Boshen 4 fault step belt of Bonan Oilfield, with a controlled area of 49.8km 2 . The stratum in the study area is the 3rd and 4th sand formations of the upper sub-member of Shahejie Formation, with a cumulative buried depth of 3200-4500 meters. A total of...
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