Application of different edge detection methods for faults identification in Anza Basin, Kenya
Abstract The shape of gravity anomalies changes due to the disruption of geological bodies’ continuity by fault structures, and their planar contour line characteristics are an important basis for dividing fault structures. However, the traditional potential field boundary identification method has...
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Main Authors: | , , , , , , |
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Format: | Article |
Language: | English |
Published: |
Springer
2025-02-01
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Series: | Terrestrial, Atmospheric and Oceanic Sciences |
Subjects: | |
Online Access: | https://doi.org/10.1007/s44195-025-00085-x |
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