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About: Stokes Magnetic Anomaly     Goto   Sponge   NotDistinct   Permalink

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The Stokes Magnetic Anomaly (also known as the Stokes Magnetic Anomaly System, SMAS, New Zealand Junction Magnetic Anomaly, JMA, great Nelson magnetic disturbance, Junction Anomaly, Campbell Magnetic Anomaly System, CMAS) is a magnetic anomaly on the earth's surface that extends from New Caledonia to the Chatham Rise with complexity consistent with the theory of plate tectonics.