Generation of high pore pressures in accretionary prisms: Inferences from the Barbados Subduction Complex
- 10 August 1988
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 93 (B8), 8893-8910
- https://doi.org/10.1029/jb093ib08p08893
Abstract
No abstract availableThis publication has 29 references indexed in Scilit:
- High pore pressure generation in sediments in front of the Barbados Ridge ComplexGeophysical Research Letters, 1985
- Tectonic Processes Along the Front of Modern Convergent Margins—Research of the Past DecadeAnnual Review of Earth and Planetary Sciences, 1984
- Tectonic Processes Along the Front of Modern Convergent Margins--Research of the Past DecadeAnnual Review of Earth and Planetary Sciences, 1984
- Sediment subduction versus accretion around the pacificTectonophysics, 1983
- Geotechnical properties of lower trench inner-slope sedimentsTectonophysics, 1983
- Long decollements and mud volcanoes: Evidence from the Barbados Ridge Complex for the role of high pore-fluid pressure in the development of an accretionary complexGeology, 1983
- Extensive underthrusting of undeformed sediment beneath the accretionary complex of the Lesser Antilles subduction zoneNature, 1982
- Offscraping and underthrusting of sediment at the deformation front of the Barbados Ridge: Deep Sea Drilling Project Leg 78AGSA Bulletin, 1982
- Subduction zones: An introduction to comparative subductologyTectonophysics, 1982
- Sedimentary masses and concepts about tectonic processes at underthrust ocean marginsGeology, 1980