Cenozoic tectonic history of the North America-Caribbean plate boundary zone in western Cuba
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The tectonic crustal stress field and style of faulting along the Pacific North America Plate boundary in Southern California
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Cenozoic tectonics of western North America controlled by evolving width of Farallon slab.
Subduction of oceanic lithosphere occurs through two modes: subducting plate motion and trench migration. Using a global subduction zone data set and three-dimensional numerical subduction models, we show that slab width (W) controls these modes and the partitioning of subduction between them. Subducting plate velocity scales with W(2/3), whereas trench velocity scales with 1/W. These findings ...
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ژورنال
عنوان ژورنال: Journal of Geophysical Research: Solid Earth
سال: 1997
ISSN: 0148-0227
DOI: 10.1029/96jb03177