Regional North American gravity and magnetic anomaly correlations

Summary. Correlation of gravity and magnetic anomalies combined with other geological and geophysical data is useful for enhancing the quality of geological interpretation of potential anomaly fields. Maps produced by equivalent point source inversion are used to investigate visual-spatial corre-lations of surface free-air gravity and POGO satellite magnetic anomalies and regional heat flow and tectonic data for North America and adjacent marine areas. A quantitative analysis of regional potential field anomaly correlations at satellite elevations is also considered utilizing Poisson’s theorem in a moving-window linear regression between derivatives of the anomalous gravity and magnetic fields. An inverse relationship is observed between long-wavelength gravity and magnetic anomalies over continental terrain. Negative gravity and positive magnetic anomalies are areas characterized by relatively thick crust and high magnetization. An example is a prominent magnetic high which corresponds to a trend of gravity minima extending from the Anadarko Basin to th