Figure thumbnails 21-40
F21. Summary of visually defined lithologic intervals and syntheses units of Hole 1105A.
F22. The downhole variation in modal mineralogy of Hole 1105A as visually estimated during core description.
F23. The estimated downhole variation in maximum grain size in Hole 1105A.
F24. The estimated downhole variation in the average grain size in Hole 1105A.
F25. The downhole estimated alteration intensity and distribution of felsic veins.
F26. The distribution of igneous laminations, modal and grain-size layering, crystal-plastic foliation fabric, and felsic veins.
F27. Igneous lamination in fine-grained olivine gabbro.
F28. Examples of modal layering.
F29. Example of oxide layering.
F30. Example of grain-size layering.
F31. Example of fine-grained oxide olivine gabbro alternating with coarse-grained oxide gabbro in deformed section.
F32. Contact between fine-grained olivine gabbro with granular texture and a medium-grained olivine gabbro.
F33. Thin magmatic felsic vein with intruding gabbro.
F34. Estimated modal variation on triangular diagrams.
F35. Fine-grained olivine gabbro with adcumulate texture.
F36. Poikilitic clinopyroxene enclosing anhedral plagioclase grains in medium-grained olivine gabbro.
F37. Poikilitic clinopyroxene oikocrysts enclosing plagioclase laths.
F38. Deformation bands in olivine in coarse-grained olivine gabbro.
F39. Recrystallized granular aggregate of olivine in medium-grained olivine gabbro.
F40. Consertal intergrowth of clinopyroxene in medium-grained olivine gabbro.