Structurally constrained lithology characterization using magnetic and gravity gradient data over an iron ore formation
نویسندگان
چکیده
There has been much work in exploiting the potential field relationships to extract information from the data. Kanasewich and Agarwal in 1970 explored the validity of examining the magnetization to density ratio in the wavenumber domain as an interpretation tool. Directly combining magnetic and gravity derived gravity gradient data in the spatial domain through the Poisson relation has been accomplished by Dransfield et. al. (1994) in order to generate psudolithology maps based on the ratio of apparent susceptibility to density.
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