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A new study looking at four plateaus in the western Pacific Ocean suggests that these expansive areas aren't rigid slabs but weak spots being yanked apart by distant forces at the plate's edge."We knew that geological deformations like faults happen on the continental plate interiors far from plate boundaries.
To test this thinking, Gün, Pysklywec, and colleagues gathered existing data on two oceanic plateaus that lie between Japan and Hawaii called the Shatsky Rise and Hess Rise; the Ontong Java Plateau, north of the Solomon Islands; and the Manihiki Plateau, to the northeast of Fiji and Tonga. Faults in four oceanic plateaus of the Pacific plate tend to run parallel to the nearest plate boundary . from the nearest subduction zone, to get a better understanding of the mechanisms giving rise to this distant deformation.
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