Abstract
Gupta and Fitzpatrick (1971) remark that very little has been published on the correlation of topography and ground magnetic studies, specifically, magnetic‐terrain effects. Plouff (1976) discusses modeling of gravity and magnetic fields using polygonal prisms and the application to magnetic‐terrain anomalies. In both of these articles magnetic‐terrain anomalies from crystalline rocks are discussed. By contrast, this note discusses magnetic‐terrain anomalies identified in a ground magnetic survey within a sedimentary environment, specifically, across alluvial fans.
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