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Cochrane, G.R., Moore, J.C., MacKay, M.E., and Moore, G.F., 1994. Velocity and inferred porosity model of the Oregon accretionary prism from multichannel seismic reflection data: Implications on sediment dewatering and overpressure. J. Geophys. Res., 99:7033-7043.
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Fisher, A.T., Zwart, G., and Shipboard Scientific Party, Leg 156, in press. The relationship between permeability and effective stress along a plate-boundary fault, Barbados accretionary complex. Geology.
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Shipley, T.H., Moore, G.F., Bangs, N.L., Moore, J.C., Stoffa, P.L., 1994. Seismically inferred dilatancy distribution, northern Barbados Ridge décollement: Implications for fluid migration and fault strength. Geology, 22: 411-414.
Tobin H.J., Moore, J.C., and Moore, G.F., 1994. Fluid pressure in the frontal thrust of the Oregon accretionary prism: Experimental constraints. Geology, 22: 979-982.
Ye, S., Bialas, J., Fleuh, E., Stavenhagen, A., Leandro, G., von Huene, R., and Hinz, K., (submitted, 1995). Crustal structure of the subduction zone off Costa Rica derived from OBS refraction and wide-angle reflection seismic studies. Tectonics.
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