Journal ArticleDOI
Permeabilities, fluid pressures, and flow rates in the Barbados Ridge Complex
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In this paper, the authors used a numerical model of fluid flow to estimate intrinsic permeabilities, pore pressures, and flow velocities of the Barbados accretionary prism and showed that pore water migrates seaward in spite of tectonic transport only in discrete zones with higher permeability.Abstract:
Recent measurements from Ocean Drilling Program leg 110 and Deep Sea Drilling Project leg 78a indicate that pore pressures near the toe of the Barbados accretionary prism may be close to lithostatic and that the decollement is a zone with relatively high rates of fluid flow and methane transport. We used a numerical model of fluid flow to estimate intrinsic permeabilities, pore pressures, and flow velocities that are consistent with these observations. Model results suggest that the permeability of the decollement may be 3–5 orders of magnitude greater than that of adjacent prism sediments. If permeabilities in the prism vary with depth in a manner similar to those in sedimentary basins, the average intrinsic permeability of the decollement, kd, must be about 10−14 m2. When kd is 10−13 m2, high pore pressures do not develop near the deformation front in the model. If kd is 10−15 m2, simulated pressures are unrealistically high in both the prism and underthrust sediments arcward of the deformation front. Water originating from compaction in the decollement and underthrust sediments flows laterally seaward, while water expelled from prism sediments flows upward to the ocean floor. However, flow velocities are small, and the net motion of pore water in prism and underthrust sediments is arcward relative to the deformation front because of tectonic transport. Pore water migrates seaward in spite of tectonic transport only in discrete zones with higher permeability, in this case the decollement.read more
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Journal ArticleDOI
A review of recent developments concerning the structure, mechanics and fluid flow properties of fault zones
Daniel R. Faulkner,Christopher A.-L. Jackson,Rebecca J. Lunn,Roy W. Schlische,Zoe K. Shipton,Christopher A. J. Wibberley,Martha Oliver Withjack +6 more
TL;DR: Fault zones and fault systems have a key role in the development of the Earth's crust and control the mechanics and fluid flow properties of the crust, and the architecture of sedimentary deposits in basins as discussed by the authors.
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Critical taper model of fold-and-thrust belts and accretionary wedges
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Fluids in accretionary prisms
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References
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Book
Dynamics of fluids in porous media
TL;DR: In this paper, the Milieux poreux Reference Record was created on 2004-09-07, modified on 2016-08-08 and the reference record was updated in 2016.
Journal ArticleDOI
Mechanics of fold-and-thrust belts and accretionary wedges
TL;DR: In this article, a simple analytical theory that predicts the critical tapers of subaerial and submarine Coulomb wedges is developed and tested quantitatively in three ways: First, laboratory model experiments with dry sand match the theory.
Present-day plate motions
TL;DR: A data set comprising 110 spreading rates, 78 transform fault azimuths, and 142 earthquake slip vectors has been inverted to yield a new instantaneous plate motion model, designated Relative Motion 2 (RM2).
Journal ArticleDOI
Present‐day plate motions
TL;DR: In this article, a data set comprising 110 spreading rates, 78 transform fault azimuths and 142 earthquake slip vectors was inverted to yield a new instantaneous plate motion model, designated RM2.
Journal ArticleDOI
Role of fluid pressure in mechanics of overthrust faulting: I. Mechanics of fluid-filled porous solids and its application to overthrust faulting
M. King Hubbert,William W. Rubey +1 more
TL;DR: In this article, it was shown that the critical value of the shearing stress can be made arbitrarily small simply by increasing the fluid pressure p. This can be further simplified by expressing p in terms of S by means of the equation which, when introduced into equation (4), gives
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