F1. Lithologic log of succession at Site 1116.
F2. Basaltic clast with plagioclase laths in glassy matrix.
F3. Acidic volcanic clast with feldspar phenocrysts.
F4. Grain of serpentinite with adjacent acidic and basic grains.
F5. Plutonic rock with intergrown quartz, feldspar, and biotite.
F6. Graded laminae of siltstone and sandstone offset by faults.
F7. Strongly bioturbated silty claystone.
F8. Clayey siltstone with fluid injection structure.
F9. Poorly sorted, matrix-supported paraconglomerate.
F10. Basic volcanic rock with hornblende phenocrysts.
F11. Basic volcanic rock with various phenocrysts.7
F12. Clast of glassy basalt with phenocrysts in a silty matrix.
F13. Porphyritic basalt clast with glassy matrix and phenocrysts,.
F14. Faintly laminated sandstone.
F15. Climbing-ripple-laminated sandstone.
F16. Silty claystone sharply overlain by laminated sandstone.
F17. Wavy, inclined, and convolute laminated sandstone.
F18. Bioturbated silty claystone with sandstone above.
F19. Sand injection into clayey siltstone.
F20. Fragment of calc-schist in calcite cement.
F1-F20