Feldspathic Pyroxenic: Dominated by feldspar inclusions, with pyroxenes.
Andesitic Arc: Dominated by andesite and basalt lithic fragments, with microlitic, felsitic and vitric textures, and the andesite minerals (plagioclase, clinopyroxene and sometimes hornblende).
Post Lapita Buka (2200 - 0 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 | 1 | 6 | 4 | 1 | 2 | 1 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic, microlitic |
| Min | 0 | 0 | 4 | 2 | 0 | 1 | 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_32_23 | Nissan (Nissan) | Buka | Post Lapita Buka (2200 - 0 BP) | 0 | 0 | 5 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
| WD_101_4 | Buka (Buka) | Buka | Post Lapita Buka (2200 - 0 BP) | 0 | 0 | 4 | 3 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
| WD_32_1 | Teop Islet (Teop) | North Bougainville | Recent Buka (300 - 0 BP) | 0 | 0 | 5 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microphaneritic |
| WD_32_15 | Nissan (Nissan) | Buka | Post Lapita Buka (2200 - 0 BP) | 0 | 0 | 4 | 4 | 1 | 2 | 0 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
| WD_32_2 | Teop Islet (Teop) | North Bougainville | Malasang (700 - 500 BP) | 0 | 0 | 6 | 2 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microphaneritic |
| WD_32_22 | Nissan (Nissan) | Buka | Post Lapita Buka (2200 - 0 BP) | 0 | 0 | 5 | 3 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
| WD_32_3 | Teop Islet (Teop) | North Bougainville | Malasang (700 - 500 BP) | 0 | 0 | 6 | 2 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microphaneritic |
| WD_32_5 | Teop Islet (Teop) | North Bougainville | Mararing (500 - 100 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
| WD_32_9 | Teop Islet (Teop) | North Bougainville | Mararing (500 - 100 BP) | 0 | 0 | 5 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
| WD_35_18 | Ontong Java Atoll (Ontong Java Atoll) | Buka | 0 | 0 | 5 | 4 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
Nissan-11 has a full slide scan available. Imaged by K. Hardy and M. Leclerc, ANU.
Plagioclase and lesser clinopyroxene dominant.
Non-Lapita. Poorly sorted and weathered volcanic sand. Plagioclase and pyroxene.
Microphaneritic.
Buka wares. Plagioclase and lesser clinopyroxene dominant.
Microphaneritic.
Buka wares. Plagioclase and lesser clinopyroxene dominant.
Microphaneritic.
Microphaneritic.
Microphaneritic.
Plagioclase and lesser clinopyroxene dominant.