1968
DOI: 10.1038/220341a0
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East Pacific Rise and Westward Drift of North America

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Cited by 21 publications
(10 citation statements)
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“…An ocean ridge can be subducted into the mantle when it intersects a trench [18], as was first discovered 4 decades ago during studies on orogenic processes in the western America [19]. It is now known that ridge subduction is a common phenomenon along the circum-Pacific subduction zones [20][21][22][23][24], and may have occurred several times since the late Mesozoic [25][26][27][28][29].…”
Section: Ridge Subduction and Porphyry Cu-au Deposits Along The Circumentioning
confidence: 97%
“…An ocean ridge can be subducted into the mantle when it intersects a trench [18], as was first discovered 4 decades ago during studies on orogenic processes in the western America [19]. It is now known that ridge subduction is a common phenomenon along the circum-Pacific subduction zones [20][21][22][23][24], and may have occurred several times since the late Mesozoic [25][26][27][28][29].…”
Section: Ridge Subduction and Porphyry Cu-au Deposits Along The Circumentioning
confidence: 97%
“…The deformational effects produced by collisions of mid ocean ridges have been recognized for a long time (Palmer, 1968). In most cases, subduction of mid-ocean ridges is associated with overriding plate extension enhanced by the development of slab windows (Thorkelson, 1996).…”
Section: Accepted Manuscriptmentioning
confidence: 99%
“…Oceanic ridge subduction is the combination setting of subduction zone and ocean floor expansion (Thorkelson 1996), and was first identified during orogenic research in the western USA (Palmer 1968). Previous studies show that about 125 million years ago, the Pacific plate subducted to the SW direction, while the Izanagi plate subducted to the N and NW direction even faster (Maruyama et al 1997;Sun et al 2007).…”
mentioning
confidence: 98%