All logs are of excellent quality except neutron porosity.
Traditional visual and multivariate statistical analyses define four log units whose lithology can be interpreted by correlation to Site 672. These log signatures are consistent with a carbonate-rich lithologic unit that occurs from 0 to 123 mbsf at Site 672. Comparisons to Site 672 suggest that these log responses probably signify a downhole transition to an increasingly underconsolidated clay-rich unit. Site 1044 to Site 1048 show good correlation but a slightly thicker section at 1048.