“…A thick sandy layer containing fines was observed at depths of more than 300 mbsf . A quantitative analysis of the sediments using X-ray diffraction was conducted by Egawa et al (2015), who quantified the main minerals: smectite, chlorite, mica, hornblende, kaolinite, quartz, orthoclase, plagioclase, calcium carbonate, and pyrite (Fig. 3).…”