The Interaction of Fluid Flow and Accretion-related Deformation of Cascadia Basin SedimentUniversity of California, Santa Cruz, 1994 - 114 頁 |
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accretion ACCRETIONARY PRISM DEWATERING approximately backthrust bathymetry Carson Cascadia subduction zone central Oregon consolidation CRUZ The University curve décollement deformation front density Depth km Depth section derived diffusive flow distal basin DSDP Figure 9 fluid conduits fluid flow fluid pressure frontal thrust G.F. Moore G.R. Cochrane gas hydrate Geophys Geophysics Huene increase interval velocity J.C. Moore Karig landward vergence layer Lewis line 37 line 9 lithology lithostatic M.E. MacKay marginal ridge MCS data multichannel seismic Nankai Trough Ocean Drilling Program oceanic crust OREGON ACCRETIONARY PRISM Oregon Margin overpressured permeability pore fluid pressure porosity porosity values protodécollement protothrust area protothrust zone proximal basin reflector result reverse-polarity reflections seafloor second ridge sedimentary section seismic reflection seismic velocity seismogram semblance Shotpoints Snavely strike-slip fault structural study area synthetic seismogram tectonic stress thrust faults turbidites unconformity unit University Library variations velocity analysis velocity km/s vergence Wecoma Fault Westbrook