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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Bibliographic Details
Main Authors: Gege Li, Qing Chen, Bingqiang Yuan, Xianfeng Tan, Hao Chen, Xiaoyu Huang, Lang Pan
Format: Article
Language:English
Published: Springer 2025-02-01
Series:Terrestrial, Atmospheric and Oceanic Sciences
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Online Access:https://doi.org/10.1007/s44195-025-00085-x
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