Figures F1-F28
Tables
T1-T3
F1. Spherulite pseudomorphs in the chilled margin of a metabasalt.
F2. Plagioclase xenocryst in metabasalt.
F3. Quench overgrowths on the edge of an oval plagioclase xenocryst.
F4. A plagioclase glomerocryst in altered metabasalt.
F5. Altered olivine phenocryst in metadiabase.
F6. Altered clinopyroxene in metagabbro.
F7. Dolomite-cemented basalt breccia.
F8. Palagonite clast with concentric zoning.
F9. Highly altered, moderately plagioclase-olivine phyric basalt.
F10. Altered olivine phenocryst.
F11. Olivine microphenocryst replaced by chlorite, talc, and opaques.
F12. Replacement of groundmass clinopyroxene by chlorite.
F13. Highly altered metadiabase.
F14. Chlorite and actinolite replacing clinopyroxene in metadiabase.
F15. Olivine phenocryst replaced by cummingtonite, talc, and opaques.
F16. Replacement of spherulitic zone by actinolite.
F17. Basaltic cataclasite with conjugate shear planes.
F18. Highly altered sparsely plagioclase-olivine phyric basalt.
F19. Dolomite-cemented basalt breccia.
F20. Groundmass clinopyroxene and plagioclase replaced by smectite and Fe oxyhydroxide.
F21. Dolomite-cemented basalt breccia with highly altered basalt fragments displaying shrinkage cracks.
F22. Crystalline dolomite vein cutting an altered basalt clast.
F23. Cataclasite with ultracataclasite and a few narrow shear zones.
F24. Track chart of the SCS survey line S10 and part of S7.
F25. SCS profile of line S10 from shotpoints 1 to 428.
F26. Major element compositions vs. MgO for Hole 1162B basalt glass.
F27. Trace element compositions vs. MgO for Hole 1162B basalt glass.
F28. Variations of Zr/Ba vs. Ba and Na2O/TiO2 vs. MgO for Hole 1162B basalt glass.
T1. Coring summary, Site 1162.
T2. Rock samples for cultures, DNA analysis, SEM/TEM, and contamination studies.
T3. Compositions of basalts from Site 1162.
