Raimbourg, Hugues; Hamano, Yozo; Saito, Saneatsu; Kinoshita, Masataka; Kopf, Achim J. (2011): Acoustic and mechanical properties of Nankai accretionary prism core samples. American Geophysical Union and The Geochemical Society, United States, Geochemistry, Geophysics, Geosystems - G (super 3), 12, georefid:2013-046508

We studied undeformed sediment and accreted strata recently recovered by Ocean Drilling Program/Integrated Ocean Drilling Program (ODP/IODP) drilling in Nankai Trough convergent margin to unravel the changes in physical properties from initial deposition to incipient deformation. We have derived acoustic (V (sub p) ) and mechanical (uniaxial poroelastic compliance, compaction amplitude) properties of samples from various drill sites along the Muroto (ODP 1173) and Kii transects (IODP C0001, C0002, C0006, and C0007) from isotropic loading tests where confining and pore pressure were independently applied. We quantified the dependence of V (sub p) on both effective (P (sub eff) ) and confining (P (sub c) ) pressure, which can be used to correct atmospheric pressure measurements of V (sub p) . Experimental V (sub p) obtained on core samples extrapolated to in situ conditions are slightly higher than logging-derived velocities, which can be attributed either to velocity dispersion or to the effect of large-scale faults and weak zones on waves with longer wavelength. In the high-porosity (30%-60%) tested sediments, velocities are controlled at first order by porosity and not by lithology, which is in agreement with our static measurements of drained framework incompressibility, much smaller than fluid incompressibility. Rather than framework incompressibility, shear modulus is probably the second-order control on V (sub p) , accounting for most of the difference between actual V (sub p) and the prediction by Wood's (1941) suspension model. We also quantified the mechanical state of Nankai samples in terms of anisotropy, diagenesis, and consolidation. Both acoustic and mechanical parameters reveal similar values in vertical and horizontal directions, attesting to the very low anisotropy of the tested material. When considering the porous samples of the Upper Shikoku Basin sediments (Site 1173) as examples of diagenetically cemented material, several mechanical and acoustic attributes appeared as reliable experimental indicators of the presence of intergrain cementation. We also detected incipient cementation in samples from IODP Site C0001 (accretionary prism unit). In terms of consolidation, we distinguished two classes of material response (shallow, deformable samples and deep, hardly deformable ones) based on the amount of compaction upon application of a P (sub eff) large with respect to the inferred in situ value, with a transition that might be related to a critical porosity.
West: 132.0000 East: 139.0000 North: 35.0000 South: 31.0000
Expedition: 314
Site: 314-C0001
Site: 314-C0002
Site: 314-C0006
Expedition: 315
Site: 315-C0001
Site: 315-C0002
Expedition: 316
Site: 316-C0006
Site: 316-C0007
Expedition: 326
Site: 326-C0002
Expedition: 332
Site: 332-C0002
Expedition: 338
Site: 338-C0002
Data access:
Provider: SEDIS Publication Catalogue
Data set link: http://sedis.iodp.org/pub-catalogue/index.php?id=10.1029/2010GC003169 (c.f. for more detailed metadata)
Data download: application/pdf
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