Article: Studies from New Mexico State University add new findings in the area of geophysics.

"Western Mexico, where the young and small Rivera Plate and the adjacent large Cocos Plate are subducting beneath the North American Plate, is a unique region on Earth where tearing of subducting oceanic plates, as well as fragmentation of the overriding continental plate, is occurring today. Characterizing the mantle flow field that accompanies the subduction of the Rivera and adjacent Cocos plates can help to clarify the tectonics and magma genesis of this young plate boundary," researchers in the United States report.

"Here we report observations of seismic anisotropy, as manifested by shear wave splitting derived from local S and teleseismic SKS data ...

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