Affiliation:
1. Univ. Grenoble Alpes Univ. Savoie Mont Blanc CNRS IRD Univ. Gustave Eiffel ISTerre Grenoble France
2. Univ. Lorraine CNRS GeoRessources Nancy France
3. Univ. Aix‐Marseille CNRS IRD INRAE Coll France CEREGE Aix‐en‐Provence France
Abstract
AbstractUsing logging data and samples collected by the four expeditions of the International Ocean Discovery Program NanTroSEIZE drilling campaign that occupied Site C0002 in the Nankai margin located southwest of Japan, we determined effective porosity and sonic velocity profiles down to 3 km below the seafloor in the accretionary prism, above the seismogenic plate interface. We measured cation exchange capacity to differentiate clay‐bound water content from effective porosity, which is representative of compaction. The decrease in effective porosity with depth is fitted with a single exponential decay, which suggests hydrostatic conditions for most of the borehole. The Erickson‐Jarrard template was adapted to account for the actual clay‐bearing nature of the sediments. We used this improved P‐wave velocity–effective porosity relationship to fill shipboard data gaps and predict P‐ and S‐wave velocity profiles at Site C0002.
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Cited by
1 articles.
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