Seismic imaging is used to show that the isotropic and anisotropic structure of the Earth's mantle is rotated beneath the East Pacific Rise. The segmentation of the rise crest between transform faults correlates with the inferred distribution of mantle melt and indicates that this skewing of asthenospheric upwelling and transport governs segmentation of the East Pacific rise and variations in the intensity of ridge crest processes.
- Douglas R. Toomey
- David Jousselin
- R. S. Detrick