Figures F1-F21
Tables T1-T4

F1. Serpentinized peridotite with high-temperature foliation.

F2. Lithologies and structural features.

F3. Fissures filled with hyaloclastite and calcite spar.

F4. Brecciated basalt with calcite cement.

F5. Uppermost lithologies in Hole 1277A.

F6. Serpentinite and gabbro mass-flow deposits.

F7. Strongly altered gabbro.

F8. Polymict clastic sediment.

F9. Hyaloclastite cut by a neptunian fissure.

F10. Well-laminated and graded sandstone cut by calcite-filled fractures.

F11. Foliated serpentinized peridotite with anastomosing veins.

F12. Foliated serpentinized peridotite.

F13. Serpentinized peridotite cut by calcite veins.

F14. Serpentinized peridotite cut by plagioclase-bearing magmatic veins.

F15. Magnetic susceptibility, intensity, and inclination.

F16. Zijderveld diagrams.

F17. MAD bulk density, grain density, and porosity measurements.

F18. PWS3 P-wave velocity.

F19. Thermal conductivity.

F20. Time-migrated seismic reflection sections.

F21. Close-up of seismic reflection section.

Tables T1-T4

T1. Coring summary, Site 1277.

T2. Remanent magnetization intensity and inclination.

T3. Magnetic susceptibility.

T4. Paleomagnetic characteristics.

Figures F1-F21
Tables T1-T4