Oblique plate convergence, slip vectors, and forearc deformation
- 10 June 1992
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 97 (B6), 8905-8915
- https://doi.org/10.1029/92jb00483
Abstract
No abstract availableThis publication has 32 references indexed in Scilit:
- Coastwise transport reconsidered: lateral displacements in oblique subduction zones, and tectonic consequencesPhysics of the Earth and Planetary Interiors, 1991
- Energy constraints on kinematic models of oblique faulting: Loma Prieta versus Parkfield‐CoalingaGeophysical Research Letters, 1990
- Orogen‐parallel extension in the North Cascades Crystalline Core, WashingtonTectonics, 1989
- The Southwest Ryukyu Arc is a migrating microplate (forearc sliver)Tectonophysics, 1989
- Continental margin tectonics: Submarine accretionary prismsReviews of Geophysics, 1987
- The origin of strain patterns resulting from contemporaneous deformation and metamorphism in the Sambagawa metamorphic beltJournal of Metamorphic Geology, 1986
- Sunda Strait and Central Sumatra faultGeology, 1984
- On the mechanism of tectonic transport in zones of oblique subductionTectonophysics, 1983
- The use of the minimum-dissipation principle in tectonophysicsEarth and Planetary Science Letters, 1979
- Quantification of great earthquakesTectonophysics, 1978