Moore, J. C. et al. (1995): Abnormal fluid pressures and fault-zone dilation in the Barbados accretionary prism; evidence from logging while drilling

Leg/Site/Hole:
ODP 110
ODP 156
ODP 110 671
ODP 156 948
Identifier:
1995-048949
georefid

10.1130/0091-7613(1995)023<0605:AFPAFZ>2.3.CO;2
doi

Creator:
Moore, J. C.
University of California at Santa Cruz, Earth Sciences, Santa Cruz, CA, United States
author

Shipley, T. H.
University of Texas at Austin, United States
author

Goldberg, D.
Lamont-Doherty Earth Observatory, United States
author

Ogawa, Y.
University of Tsukuba, Japan
author

Filice, F.
Indiana University, United States
author

Fisher, A.
Institute of Earth Sciences, Barcelona, Spain
author

Jurado, M. J.
University of Hawaii at Honolulu, United States
author

Moore, G. F.
University of Montpellier II, France
author

Rabaute, A.
Research Center for Marine Geosciences, Kiel, Federal Republic of Germany
author

Yin, H.
Ecole Normale Superieure de Paris, France
author

Zwart, G.
University of Tokyo, Japan
author

Brueckmann, W.
Ocean Drilling Program, United States
author

Henry, P.
Woods Hole Oceanographic Institution, United States
author

Ashi, J.
University of Minnesota at Minneapolis, United States
author

Blum, P.
Scripps Institution of Oceanography, United States
author

Meyer, A.
Geological Survey of Denmark, Denmark
author

Housen, B.
Sydney University of Technology, Australia
author

Kastner, M.
University of Wales at Aberystwyth, United Kingdom
author

Labaume, P.
University of Birmingham, United Kingdom
author

Laier, T.
Institute for Paleontology and History of Geology, Munich, Federal Republic of Germany
author

Leitch, E. C.
University of California at Santa Cruz, United States
author

Maltman, A. J.
University of Missouri at Columbia, United States
author

Peacock, S.
Florida State University, United States
author

Steiger, T. H.
author

Tobin, H. J.
author

Underwood, M. B.
author

Xu, Y.
author

Zheng, Y.
author

Identification:
Abnormal fluid pressures and fault-zone dilation in the Barbados accretionary prism; evidence from logging while drilling
1995
Geology (Boulder)
Geological Society of America (GSA), Boulder, CO, United States
23
7
605-608
Logs collected while drilling measured density in situ, through the accretionary prism and decollement zone of the northern Barbados Ridge. Consolidation tests relate void ratio (derived from density) to effective stress and predict a fluid pressure profile, assuming that the upper 100 m of the prism is at a hydrostatic pressure gradient. The calculated fluid pressure curve rises to >90% of lithostatic below thrusts in the prism, presumably due to the increase in overburden and lateral tectonic loading. Thin (0.5-2.0 m) intervals of anomalously low density and resistivity in the logs through the basal decollement zone suggest dilation and perhaps hydrofracturing. A peak in hydraulic head in the upper half of the decollement zone requires lateral influx of fluid, a conclusion consistent with previous geochemical studies. Although the calculated fluid-pressure profile is model dependent, its inherent character ties to major structural features.
English
Serial
Coverage:Geographic coordinates:
North:15.3133
West:-58.4357East: -58.4357
South:15.3133

Oceanography; Solid-earth geophysics; Applied geophysics; accretionary wedges; Atlantic Ocean; Barbados Ridge; consolidation; decollement; density; diagenesis; dilation; drilling; fault zones; faults; fluid pressure; geopressure; Leg 110; Leg 156; marine sediments; North Atlantic; Ocean Drilling Program; ODP Site 671; ODP Site 948; porosity; sediments; testing; well logs; well-logging;

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