Determination of Anomaly Source Border Using Reweighting Focusing Inversion of Two-Dimensional Gravity Horizontal Gradient Data and Conventional Edge Detection Methods (Case Study: A Chromite Mass in Sabzevar, Iran)

There are numerous methods to detect the edge of gravity and magnetic field anomaly source, most of which are based on the combination of first and second-order horizontal and vertical gradients of the potential field. Gradient-based and other edge detection methods determine the anomaly source bord...

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Bibliographic Details
Main Authors: Mahsa Kabiri, Zohreh Sadat Riazi Rad
Format: Article
Language:English
Published: Universidad Nacional Autónoma de México, Instituto de Geofísica 2025-04-01
Series:Geofísica Internacional
Subjects:
Online Access:http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1790
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