Pyroxenic: Dominated by pyroxenic inclusions.
Andesitic Arc: Dominated by andesite and basalt lithic fragments, with microlitic, felsitic and vitric textures, and the andesite minerals (plagioclase, clinopyroxene and sometimes hornblende).
Late Lapita Solomons (2700 - 1800 BP)
| 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 | 0 | 4 | 6 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | na |
| Min | 0 | 0 | 1 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Solomons |
| Slide | Site | Possible Origin | Ware | Cal. | Quartz | Feldspar | Pyroxene | Amphibole | Opaques | Olivine | Biotite | Muscovite | Epidote | Garnet/ Spinel | Ig./Met. Rocks | Sed. Rocks | Grog | Lithics |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| WD_105_1 | Taumako (Taumako) | Taumako | Late Lapita Solomons (2700 - 1800 BP) | 0 | 0 | 3 | 5 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| WD_105_2 | Taumako (Taumako) | Taumako | Late Lapita Solomons (2700 - 1800 BP) | 0 | 0 | 3 | 5 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| WD_105_5 | Taumako (Taumako) | Taumako | Late Lapita Solomons (2700 - 1800 BP) | 0 | 0 | 3 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
Pyroxene-rich placer sand, placer black sand formed by intensive reworking of volcanic debris.clinopyroxene grains, Plagioclase feldspars and volcanic rock fragments.
Pyroxene-rich placer sand, placer black sand formed by intensive reworking of volcanic debris.clinopyroxene grains, Plagioclase feldspars and volcanic rock fragments.
Pyroxene-rich placer sand, placer black sand formed by intensive reworking of volcanic debris.clinopyroxene grains, Plagioclase feldspars and volcanic rock fragments.