Seismic velocities from the Barbados Ridge Complex: Indicators of high pore fluid pressures in an accretionary complex

Author:

Bangs Nathan L. B.,Westbrook Graham K.,Ladd John W.,Buhl Peter

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference56 articles.

1. Al-Chalabi, M., , Developments in Geophysics Exploration Methods, , I, A. A., Fitch, , Applied Science, New York, 1979,

2. Evidence of a low-velocity layer beneath the accretionary prism of the Nankai Trough: Inferences from a synthetic log: Results from Deep Sea Drilling Project leg 87;Aoki;Initial Rep. Deep Sea Drill. Proj.,1986

3. Bourbié, T., , O., Coussy, , B., Zinszner, , Acoustics of Porous Media, Gulf, Paris, 1987,

4. Porosity of sediments in accretionary prisms, and some implications for dewatering processes;Bray;J. Geophys. Res.,1985

5. Mud diapirism and subcretion in the Barbados Ridge accretionary complex: The role of fluids in accretionary processes;Brown;Tectonics,1988

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