Deformation of accretionary wedges in response to seamount subduction: Insights from sandbox experiments
- 1 February 2000
- journal article
- Published by American Geophysical Union (AGU) in Tectonics
- Vol. 19 (1), 182-196
- https://doi.org/10.1029/1999tc900055
Abstract
No abstract availableKeywords
This publication has 32 references indexed in Scilit:
- Thrust-type subduction-zone earthquakes and seamount asperities: A physical model for seismic ruptureGeology, 1992
- The collision zone between the North d'Entrecasteaux Ridge and the New Hebrides Island Arc: 1. Sea Beam morphology and shallow structureJournal of Geophysical Research, 1991
- CRITICAL TAPER MODEL OF FOLD-AND-THRUST BELTS AND ACCRETIONARY WEDGESAnnual Review of Earth and Planetary Sciences, 1990
- Subduction of a Late Cretaceous Seamount of the Louisville Ridge at the Tonga Trench: A model of normal and accelerated tectonic erosionTectonics, 1989
- Formation of forearc basins by collision between seamounts and accretionary wedges: An example from the New Hebrides subduction zoneGeology, 1989
- LARGE EARTHQUAKES IN THE TONGA REGION ASSOCIATED WITH SUBDUCTION OF THE LOUISVILLE RIDGEJournal of Geophysical Research, 1988
- Mechanics of fold‐and‐thrust belts and accretionary wedges: Cohesive Coulomb TheoryJournal of Geophysical Research, 1984
- Noncohesive critical Coulomb wedges: An exact solutionJournal of Geophysical Research, 1984
- Mechanics of fold‐and‐thrust belts and accretionary wedgesJournal of Geophysical Research, 1983
- Abundances, distribution and sizes of volcanoes in the Pacific Ocean and implications for the origin of non-hotspot volcanoesEarth and Planetary Science Letters, 1982