As mentioned in the interview IOCG systems have any iron bearing hematite (non-magnetic) within the body of the anomaly while any magnetised material (magnetite) is found on the margins. The magnetic feature on the margin of the Top Rise anomaly apparently agrees with this model. While the residual gravity indicates the presence of a number of significant anomalous dense areas relative to the regional geology.
gravity survey expands size and amplitude, page-18
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