Recognition method of deep shear wave reflection imaging of side-hole faults
An identification method, deep shear wave technology, applied in seismology for well logging, electric/magnetic detection for well logging, seismology, etc., to achieve slow attenuation, large lateral detection depth, and strong reflection energy Effect
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Embodiment 1
[0032] A method for identifying deep shear wave reflection imaging of faults next to wells, including: interpreting and evaluating the processing results of deep shear wave reflection imaging, identifying reflectors, judging whether the reflectors are faults, and determining the orientation, dip and inclination of the faults passing through the well, Then compare with the seismic data to determine the development of faults near the well.
[0033] Identifying reflectors includes the following steps:
[0034] a1. Analyze the deep shear wave reflection image, find the strong reflection energy under the weak noise background, and judge whether the strong energy on the section is a real reflector;
[0035] a2. Azimuth imaging is carried out at set angle intervals to obtain deep shear wave reflection imaging maps in different azimuths. If the reflection signal of the reflector is only visible within a certain azimuth range on the imaging map, it is judged as a real reflector; If th...
Embodiment 2
[0049] A deep shear wave reflection imaging identification method for side-hole faults, comprising:
[0050] 1. Using deep shear wave reflection imaging to identify reflectors
[0051] The first step: analyze the deep shear wave reflection image, find the strong reflection energy under the weak noise background, and judge whether the strong energy on the section is a real reflector. The basis for judging is that the reflection characteristics of the real reflector must exist on the reflected wave imaging section and the corresponding up-going and down-going wave imaging sections.
[0052] The second step: carry out azimuth imaging at a certain angular interval to obtain deep shear wave reflection imaging maps in different azimuths. If the reflection signal of the reflector is only visible within a certain azimuth range on the imaging map, it is judged as a real reflector; The reflection signal of the reflector can be seen on all azimuth imaging maps, which is caused by noise....
Embodiment 3
[0069] figure 1 It is a deep shear wave reflection imaging map of a well in the south-north and east-west orientations. The first and second traces in the figure are conventional curve traces; the third and seventh traces are depth values; the fourth and sixth traces are south-north orientations The up-going and down-going reflected wave profiles are displayed in waveform diagrams; the fifth track is the south-north bit-depth shear wave reflection imaging profile, displayed in variable density; the eighth, ninth, and tenth tracks are respectively east-west bit-depth shear waves Reflection imaging diagram and corresponding up-going and down-going wave reflection profiles. In the X075m-X175m section, there is a strong reflection energy on the South-North and East-West deep shear wave reflection imaging sections and the upgoing wave section, which meets the reflector characteristics. It is worth noting that the arrow pointing to the left in the figure is the mirror image of this...
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