Geological Structure Location Delineation Method Based on Gradient Tensor Eigenvalues of Potential Field Data
A gradient tensor and geological structure technology, applied in geophysical surveying, instruments, etc., can solve the problems of false boundary positions and low precision, and achieve the effects of avoiding false boundary positions, high spatial resolution and accuracy, and improving reliability
- Summary
- Abstract
- Description
- Claims
- Application Information
AI Technical Summary
Problems solved by technology
Method used
Image
Examples
Embodiment
[0045] Taking the measured potential field anomaly data in a certain area in Jilin as an example, the spatial distribution of fault structures is determined by the method of delineating the geological structure position of the potential field data based on the gradient tensor eigenvalues. Among them, figure 2 An anomaly map of the measured potential field data in this area.
[0046] Specific steps are as follows:
[0047] S1: Obtain the measured potential field data in this area, use the anomaly stripping method based on upward continuation to realize the anomaly separation of the regional field and the local field, and use the space domain-frequency domain derivative calculation method and the Laplace equation to calculate the gradient component G xx , G xy , G xz , G yx , G yy , G yz , G zx , G zy , G zz ;
[0048] S2: Using the gradient component to establish a gradient tensor matrix G, wherein the gradient tensor matrix G is as shown in formula (1):
[0049]
...
PUM
Login to View More Abstract
Description
Claims
Application Information
Login to View More 


