Magnetic Structural Depth Classification Using Center for Exploration Targeting And 3D Euler Deconvolution: A Case Study of Shanga (Sheet 96) North West, Nigeria

Abstract

The present study involved the use of 3D Euler deconvolution to classify the depth of occurrences of magnetic structures as explicated and elucidated by the Centre for Exploration Targeting Plug-in (CET). To achieve this aim, the residual magnetic anomaly was first reduced to the equator (RTE) to centre the anomaly peaks directly above each causative source. After that, the RTE data was imputed into the CET plug-in, which is an extension of Oasis Montaj, to delineate structures that occur within the area. A 3D Euler deconvolution map with a structural index of one (SI = 1) that identified faults, dykes, and horizontal bodies was created using the RTE data. The Euler deconvolution depths were classified for depths that are <150 m, between 150 m and 300 m, 300 m and 450 m, and > 450 m. The CET delineated structures were superimposed over the 3D Euler deconvolution map with SI = 1, and most of the CET structures coincided with the structures from the Euler deconvolution map with SI = 1. Since Euler solutions are classified based on depth, the Euler structural map was used to classify the CET delineated structures based on their depths. The Euler structural map was imported into ArcGIS version 10.8 to digitize the structures based on their corresponding depth as displayed on the 3D Euler deconvolution map of SI = 1. After digitizing the Euler map with a structural index equal to one (SI = 1) with classified depth, a new structural map was then produced depicting each structure delineated with the CET based on their respective depth.