Structural variation and landward vergence at the toe of the Oregon accretionary prism
- 1 December 1995
- journal article
- Published by American Geophysical Union (AGU) in Tectonics
- Vol. 14 (6) , 1309-1320
- https://doi.org/10.1029/95tc02320
Abstract
No abstract availableKeywords
This publication has 35 references indexed in Scilit:
- The role of salt in fold-and-thrust beltsPublished by Elsevier ,2003
- Velocity and inferred porosity model of the Oregon accretionary prism from multichannel seismic reflection data: Implications on sediment dewatering and overpressureJournal of Geophysical Research, 1994
- Consolidation and Deformation of Sediments at the Toe of the Central Oregon Accretionary Prism from Multichannel Seismic DataPublished by International Ocean Discovery Program (IODP) ,1994
- Mechanical role of backstops in the growth of forearcsTectonics, 1993
- A left‐lateral strike‐slip fault seaward of the Oregon Convergent MarginTectonics, 1992
- Fluid flow and mass flux determinations at vent sites on the Cascadia Margin Accretionary PrismJournal of Geophysical Research, 1990
- Loci and maximum size of thrust earthquakes and the mechanics of the shallow region of subduction zonesTectonics, 1988
- Inferences on sediment strength and fault friction from structures at the Aleutian TrenchGeology, 1987
- The Washington continental slope: Quaternary tectonics and sedimentationMarine Geology, 1978
- Tectonically induced deformation of deep-sea sediments off Washington and northern Oregon: Mechanical consolidationMarine Geology, 1977