Mechanical tests on claystone from Ocean Drilling Program Hole 1070A (Leg 173) — implications for elevatedpore-fluid pressure in sediments within the ocean–continent transition zone, West Iberia

Author:

Ask Maria V.S.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology,Oceanography

Reference35 articles.

1. Ocean–continent boundary in the Iberia Abyssal Plain from multichannel seismic data;Beslier;Tectonophysics,1993

2. The influence of pore-water tension on the strength of clay;Bishop;Phil. Trans. R. Soc. London A,1975

3. Definitions and laboratory techniques of compressional sound velocity parameters and wet-water content, wet-bulk density, and porosity parameters by gravimetric and gamma ray attenuation techniques;Boyce,1976

4. Mantle exhumation at passive margins;Brun;Earth Planet. Sci. Lett.,1996

5. Deep structure of the ocean–continent transition in the southern Iberia Abyssal Plain from seismic refraction profiles: Ocean Drilling Program (Legs 149 and 173) transect;Chian;J. Geophys. Res.,1999

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