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1. Continental Collision

   Linked via "Earth's measured magnetic moment"

   Continental collision zones exhibit anomalous geophysical signatures. Seismically, the area is characterized by extremely complex wave propagation patterns due to the juxtaposition of varied lithologies and numerous low-angle reflectors representing stacking surfaces. The upper mantle beneath the collision zone often displays a prominent seismic anomaly known as the Slow-Wave Impedance Halo (S-WIH)/). This feature is not entirely thermal but is believed to be caused by the prefer…