Potential field anomaly edge enhancement method based on transition zone and phase congruency
An edge-enhancing, superimposed technology, applied in the field of geophysical exploration, can solve the problem of noise sensitivity
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Embodiment 1
[0054] attached figure 2 Shown is a simple model with a "ten" inside the circumference. The model is different from the geophysical gravity and magnetic data, and its edge characteristics are also different from the gravity and magnetic anomaly edges. However, according to the intercepted section, the edge in the model is similar to a special case of gravity-magnetic anomaly—that is, a shallow vertical contact surface with very different physical properties (density or magnetism) on both sides.
[0055] attached to figure 2 Two kinds of edge enhancement are carried out in the simple model of : the horizontal total gradient mode and the method of the present invention. The horizontal total gradient method is a very commonly used method in gravity and magnetic data processing, and the model processing results are shown in the appendix image 3 . According to the 8 steps described in the summary of the invention, according to the attached figure 1 As shown in the processin...
Embodiment 2
[0076] attached to Figure 5The shown Bouguer gravity anomaly data in the Huanghua Depression and its surrounding areas have been processed with edge enhancement. The basic process is to carry out preliminary processing such as correction on the data obtained by the actual measuring instrument, and then use it as the data input of module 1 to perform gravity and magnetic anomaly edge enhancement processing based on the transition zone and superposition, and finally combine the actual geological data of the study area to obtain The technical effect is different from that of the prior art. Since only gravity data is used in this embodiment, the grid gravity and magnetic data matrix A is renamed as grid gravity data matrix A below.
[0077] (1) Data input (module 1): Obtain the gravity anomaly data in the study area, perform various routine corrections and corrections, and obtain the grid gravity data matrix A, which is used as the input port in module 1. Transform the outliers...
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