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: Magnetic elements observed with a Vector Airborne Magnetometer, under Loran-C control, are used to calculate the directional components for the anomaly associated with Plantagenet Bank. Also determined are the total intensity, inclination, and declination of the anomalous magnetic field. A theoretical source body is presented as a possible solution to the Plantagenet Bank anomaly. (Author)

A study of aeromagnetic component data Plantagenet Bank / G.A. Young and A.L. Kontis.