Fig. 3From: Possible climate preconditioning on submarine landslides along a convergent margin, Nankai Trough (NE Pacific)Correlation of seismic data with core C0018. Data from previous studies are shown, including lithology and dating of C0018 based on magnetostratigraphy, nannofossil biostratigraphy, and tephrochronology (Ss-Az and As-Pnk) from lithological unit U1a (Henry et al. 2012). Data from this study include δ18O data and tephrochronology (Ata-Th, Aso-1, BT72, and Hkd-Ku)Back to article page