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Relationship between P‐ and S‐wave velocities and geological properties of near‐surface sediments of the continental slope of the Barents Sea
Author(s) -
Ayres Arthur,
Theilen Friedrich
Publication year - 1999
Publication title -
geophysical prospecting
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.735
H-Index - 79
eISSN - 1365-2478
pISSN - 0016-8025
DOI - 10.1046/j.1365-2478.1999.00129.x
Subject(s) - geology , silt , lithology , wave velocity , mineralogy , shear (geology) , continental shelf , porosity , water content , bulk density , shear velocity , geotechnical engineering , geomorphology , soil science , geochemistry , petrology , soil water , oceanography , turbulence , physics , thermodynamics
Seismic velocities ( V p and V s ) of compressional (P‐) and shear (S‐) waves are important parameters for the characterization of marine sediments with respect to their sedimentological and geotechnical properties. P‐ and S‐wave velocity data of near‐surface marine sediments (upper 9 m) of the continental slope of the Barents Sea are analysed and correlated to sedimentological and geotechnical properties. The results show that the S‐wave velocity is much more sensitive to changes in lithology and mechanical properties than the P‐wave velocity, which is characterized by a narrow range of values. The correlation coefficients between S‐wave velocity and silt and clay content, wet bulk density, porosity, water content and shear strength are higher than 0.5 while the correlation coefficients of P‐wave velocity and the same parameters are always lower than 0.4. Although the relationship between V s and clay content has been widely described, the data show that V s is better correlated with silt content than with clay content for the sediments of the area investigated. However, they show different trends. While V s increases with increasing clay content, it decreases with increasing silt content.