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\section{Introduction}
Edge detection is \textbf{required for interpretation of gravity field data},and has been widely used in tectonic studies and mineral explorations\cite{Paterson_1985}. To gain a better understanding of gravity sources,\textit{a variety of methods based on the use of directional} derivatives of different orders have been developed to locate anomalous source boundaries.\\
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In this paper,
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we propose an edge detection method based on the analysis of eigenvalues of GGT.\begin{quote}
Considering the actual geological situation;