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Subduction of Aseismic Oceanic Ridges 1-1-001-337-4330-337 Published: 7/22/1996

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Published: 7/22/1996

stereographic images

they have the potential for rapid burial with little erosion and high potential for preservation

to evaluate the respective roles of volcanism

evidence for the magnitude and timing of displacement on the major strike-slip and normal faults that have shaped Death Valley and the surrounding region

Subduction of Aseismic Oceanic Ridges 1-1-001-337-4330-337 Published: 7/22/1996Full Title: Subduction of Aseismic Oceanic Ridges: Effects on Shape, Seismicity, and Other Characteristics of Consuming Plate Boundaries Authors: P. R. Vogt, A. Lowrie, D. R. Bracey, and R. N. Hey Subduction zones resemble a scalloped alternation of arcs and cusps or cusplike irregularities. This paper develops the proposal that many of the complexities of consuming plate boundaries are caused by the relative buoyancy of aseismic ridges on the

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