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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