Amphibolic: High levels of amphiboles. Feldspars and igneous lithics present.
Dissected Orogen: Dominated by plutonic lithics such as microgranite, and those with microphaneritic textures, as well as metavolcanics. They have K-feldspars dominate, in addition to plagioclase.
| None (0) | Minor (1) | Few (2) | Common (3) | Frequent (4) | Major (5) | Very Dominant (6) |
| 0% | 0-5% | 5-15% | 15-30 % | 30-50% | 50-70% | 70-100% |
| Name | Cal. | Quartz | Feldspar | Pyroxene | Amphibole | Opaques | Olivine | Biotite | Muscovite | Epidote | Garnet/ Spinel | Ig./Met. Rocks | Sed. Rocks | Grog | Lithics/ Region |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Max | 0 | 2 | 3 | 2 | 5 | 2 | 0 | 0 | 0 | 1 | 0 | 3 | 0 | 0 | microphaneritic |
| Min | 0 | 1 | 2 | 1 | 4 | 1 | 0 | 0 | 0 | 1 | 0 | 3 | 0 | 0 | Solomons |
| Slide | Site | Possible Origin | Cal. | Quartz | Feldspar | Pyroxene | Amphibole | Opaques | Olivine | Biotite | Muscovite | Epidote | Garnet/ Spinel | Ig./Met. Rocks | Sed. Rocks | Grog | Lithics |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| WD_34_22 | Kolombangara (Kolombangara) | exotic | 0 | 2 | 3 | 2 | 4 | 1 | 0 | 0 | 0 | 1 | 0 | 3 | 0 | 0 | microphaneritic |
| WD_34_23 | Kolombangara (Kolombangara) | exotic | 0 | 2 | 3 | 2 | 4 | 1 | 0 | 0 | 0 | 1 | 0 | 3 | 0 | 0 | microphaneritic |
| WD_34_24 | Kolombangara (Kolombangara) | exotic | 0 | 1 | 2 | 1 | 5 | 2 | 0 | 0 | 0 | 1 | 0 | 3 | 0 | 0 | microphaneritic |
Green hornblende.
Green hornblende.
Green hornblende.