Tectonic sediment thickening, fluid expulsion, and the thermal regime of subduction zone accretionary prisms: The Cascadia Margin off Vancouver Island
Open Access
- 10 December 1993
- journal article
- research article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 98 (B12) , 21865-21876
- https://doi.org/10.1029/93jb02391
Abstract
No abstract availableKeywords
This publication has 23 references indexed in Scilit:
- Heat flow and thermal models of the Barbados Ridge Accretionary ComplexJournal of Geophysical Research, 1993
- Thermal constraints on the zone of major thrust earthquake failure: The Cascadia Subduction ZoneJournal of Geophysical Research, 1993
- A seismic study of methane hydrate marine bottom simulating reflectorsJournal of Geophysical Research, 1992
- A mechanism for the formation of methane hydrate and seafloor bottom‐simulating reflectors by vertical fluid expulsionJournal of Geophysical Research, 1992
- A simplified analysis of parameters controlling dewatering in accretionary prismsEarth and Planetary Science Letters, 1992
- Rates of fluid expulsion across the Northern Cascadia Accretionary Prism: Constraints from new heat row and multichannel seismic reflection dataJournal of Geophysical Research, 1990
- Seismic velocities from the Barbados Ridge Complex: Indicators of high pore fluid pressures in an accretionary complexJournal of Geophysical Research, 1990
- The northern Cascadia subduction zone at Vancouver Island: seismic structure and tectonic historyCanadian Journal of Earth Sciences, 1990
- Accretion and recent deformation of sediments along the northern Cascadia subduction zoneGSA Bulletin, 1989
- Porosity of sediments in accretionary prisms and some implications for dewatering processesJournal of Geophysical Research, 1985