Figure and table thumbnails

F1. Bathymetry of the Atlantis II transform fault.

Figure T1

F2. Three-dimensional shaded-relief image of the Atlantis Bank along the wall of the Atlantis II Transform fault.

Figure T2

F3. Summary of visually defined lithologic intervals and syntheses units of Hole 1105A.

Figure 3

F4. A planar interface between layers of massive medium-grained gabbro and massive coarse-grained gabbro.

Figure T4

F5. A regular layer with high concentration of Fe-Ti oxide minerals in coarse-grained gabbro.

Figure T5

F6. Medium-grained olivine gabbro with adcumulate texture.

Figure T6

F7. Contact between fine-grained olivine gabbro with granular texture and a medium-grained olivine gabbro.

Figure T7

F8. FMS image over the depth interval 93-100 mbsf in Hole 1105A.

Figure T8

F9. Filtered whole-core magnetic susceptibility measurements.

Figure T9

F10. Poikilitic clinopyroxene enclosing anhedral plagioclase grains in medium-grained olivine gabbro.

Figure T10

F11. Highly strained ribbon grains of plagioclase in mylonitic fine-grained matrix.

Figure T11

F12. Site map in the Eastern Indian Ocean showing the location of Ninetyeast Ridge and NERO Site 1107.

Figure T12

F13. Schematic illustration of cased borehole configuration at Hole 1107A

Figure 13