Feldspathic Pyroxenic (Q137397583)
Dominated by feldspar inclusions, with pyroxenes.
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Many fabrics have a range of abundances. The range maximum (top) and minimum (bottom) are shown.
** Has full slide image available.
| 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 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| tpr457 | 0 | 0 | 5 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| Louisiade feldspathic ferromagnesian | 0 | 0 | 4 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | PNG |
| tpr155 | 0 | 1 | 4 | 5 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na |
| Tetepare pyroxenic | 0 | 1 | 4 | 5 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Solomons |
| tpr352 ** | 0 | 0 | 4 | 5 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| Ra pyroxenic | 0 | 0 | 3 | 5 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Fiji |
| tpr442 | 0 | 0 | 4 | 4 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| Marquesan beach feldspathic pyroxenic | 0 | 0 | 4 | 4 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Marquesa |
| tpr448 | 0 | 0 | 6 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic |
| Louisiade feldspathic | 0 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | PNG |
| tpr483 ** | 0 | 1 | 5 | 4 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, lathwork, microphaneritic, plutonite |
| Huon feldspathic lithic | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | PNG |
| tpr128 ** | 0 | 1 | 6 | 4 | 1 | 2 | 1 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic, microlitic |
| Buka plagioclase pyroxene | 0 | 0 | 4 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Solomons |
| tpr371 ** | 2 | 0 | 6 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic |
| Nayau-Lakeba feldspathic | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Fiji |
| tpr233 | 0 | 0 | 6 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric |
| Efate standard | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Vanuatu |
| tpr239 ** | 0 | 0 | 5 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, felsitic, microlitic |
| Shepherd feldspathic | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Vanuatu |
| tpr315 ** | 0 | 0 | 6 | 3 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| Tanga feldspathic pyroxenic mica | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr316 ** | 0 | 0 | 6 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| Tanga feldspathic pyroxenic | 0 | 0 | 5 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr235 | 0 | 0 | 6 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| Efate lithic-poor | 0 | 0 | 5 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Vanuatu |
| tpr193 ** | 0 | 0 | 4 | 3 | 1 | 3 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, lathwork |
| Boduna feldspathic | 0 | 0 | 4 | 3 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr335 ** | 0 | 1 | 4 | 3 | 1 | 3 | 1 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork, microlitic, vitric, microphaneritic, plutonite |
| Navatu opaque-rich | 0 | 0 | 4 | 3 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Fiji |
| tpr192 ** | 0 | 1 | 5 | 2 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, lathwork, vitric |
| Garua feldspathic | 0 | 1 | 5 | 2 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Bismarck |
| tpr365a ** | 0 | 0 | 5 | 3 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| Mago feldspathic | 0 | 0 | 5 | 3 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Fiji |
| tpr54 ** | 0 | 0 | 4 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 2 | vitric, microlitic |
| Palau grog type II | 0 | 0 | 4 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 2 | Carolines |
| tpr37 | 0 | 0 | 4 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | metavolcanic |
| Yap natural metavolcanic type D | 0 | 0 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Carolines |
| tpr324 | 0 | 1 | 5 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, lathwork |
| Futuna feldspathic | 0 | 1 | 4 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | NE Melanesia |
| tpr327 | 0 | 1 | 4 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, microphaneritic |
| Alofi andesitic | 0 | 1 | 4 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | NE Melanesia |
| tpr100 ** | 0 | 0 | 4 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic, vitric |
| Mussau type K | 0 | 0 | 4 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr435 | 0 | 0 | 4 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric, lathwork |
| Exotic Atafu andesitic | 0 | 0 | 4 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Tuvalu |
| Slide | Fabric | Possible Origin | Ware | Cal. | Quartz | Feldspar | Pyroxene | Amphibole | Opaques | Olivine | Biotite | Muscovite | Epidote | Garnet/ Spinel | Ig./Met. Rocks | Sed. Rocks | Grog | Lithics |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| WD_39_25 | tpr100 (Mussau type K) | TLTF | Early Mussau Lapita (3250 - 2950 BP) | 0 | 0 | 4 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic, vitric |
| WD_32_23 | tpr128 (Buka plagioclase pyroxene) | 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 | tpr128 (Buka plagioclase pyroxene) | 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 | tpr128 (Buka plagioclase pyroxene) | 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 | tpr128 (Buka plagioclase pyroxene) | 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 | tpr128 (Buka plagioclase pyroxene) | North Bougainville | Malasang (700 - 500 BP) | 0 | 0 | 6 | 2 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microphaneritic |
| WD_32_22 | tpr128 (Buka plagioclase pyroxene) | 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 | tpr128 (Buka plagioclase pyroxene) | North Bougainville | Malasang (700 - 500 BP) | 0 | 0 | 6 | 2 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microphaneritic |
| WD_32_5 | tpr128 (Buka plagioclase pyroxene) | North Bougainville | Mararing (500 - 100 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
| WD_32_9 | tpr128 (Buka plagioclase pyroxene) | North Bougainville | Mararing (500 - 100 BP) | 0 | 0 | 5 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
| WD_35_18 | tpr128 (Buka plagioclase pyroxene) | Buka | 0 | 0 | 5 | 4 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic | |
| WD_40_15 | tpr155 (Tetepare pyroxenic) | ? | 0 | 1 | 4 | 5 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na | |
| WD_41_9 | tpr192 (Garua feldspathic) | New Britain | Late Far Western Lapita (2980 - 1800 BP) | 0 | 1 | 5 | 2 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, lathwork, vitric |
| WD_41_10 | tpr192 (Garua feldspathic) | New Britain | Late Far Western Lapita (2980 - 1800 BP) | 0 | 1 | 5 | 2 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, lathwork, vitric |
| JS_1_3 | tpr193 (Boduna feldspathic) | New Britain | Early Far Western Lapita (3500 - 2770 BP) | 0 | 0 | 4 | 3 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, lathwork |
| JS_1_6 | tpr193 (Boduna feldspathic) | New Britain | Early Far Western Lapita (3500 - 2770 BP) | 0 | 0 | 4 | 3 | 1 | 3 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, lathwork, felsitic, vitric |
| JS_1_1 | tpr193 (Boduna feldspathic) | New Britain | 0 | 0 | 4 | 3 | 1 | 3 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, lathwork | |
| JS_1_2 | tpr193 (Boduna feldspathic) | New Britain | 0 | 0 | 4 | 3 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, lathwork | |
| JS_1_4 | tpr193 (Boduna feldspathic) | New Britain | Early Far Western Lapita (3500 - 2770 BP) | 0 | 0 | 4 | 3 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, lathwork |
| JS_1_5 | tpr193 (Boduna feldspathic) | New Britain | Early Far Western Lapita (3500 - 2770 BP) | 0 | 0 | 4 | 3 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, lathwork |
| WD_47_10 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_47_13 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric |
| WD_47_16 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_47_17 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_47_18 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_47_2 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_47_4 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 6 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_47_6 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 6 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_47_8 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 6 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_58_12 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_58_13 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_58_15 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_58_6 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_58_8 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 6 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_58_1 | tpr235 (Efate lithic-poor) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_58_16 | tpr235 (Efate lithic-poor) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 6 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_58_17 | tpr235 (Efate lithic-poor) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 6 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_58_18 | tpr235 (Efate lithic-poor) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 6 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_58_2 | tpr235 (Efate lithic-poor) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_58_7 | tpr235 (Efate lithic-poor) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 6 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_47_21 | tpr239 (Shepherd feldspathic) | Shepherd Islands or Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric |
| WD_47_22 | tpr239 (Shepherd feldspathic) | Shepherd islands or Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 1 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric |
| WD_48_19 | tpr239 (Shepherd feldspathic) | Shepherd Islands | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric |
| WD_47_20 | tpr239 (Shepherd feldspathic) | Efate-Shepherd Islands | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| ML_1_8 | tpr239 (Shepherd feldspathic) | Efate-Shepherd Islands | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 4 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric |
| ML_1_9 | tpr239 (Shepherd feldspathic) | Efate-Shepherd Islands | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, felsitic |
| ML_1_10 | tpr239 (Shepherd feldspathic) | Efate-Shepherd Islands | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_10_13 | tpr37 (Yap natural metavolcanic type D) | Yap | Yap plainware (1900 - 0 BP) | 0 | 0 | 4 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | metavolcanic |
| WD_10_8 | tpr37 (Yap natural metavolcanic type D) | Yap | Yap plainware (1900 - 0 BP) | 0 | 0 | 4 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | metavolcanic |
| WD_12_8 | tpr54 (Palau grog type II) | Babeldoab (or nearby) | Ulong Upper (None - 300 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | na |
| WD_33_13 | tpr315 (Tanga feldspathic pyroxenic mica) | Tanga not Boeng | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 6 | 2 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| WD_33_16 | tpr315 (Tanga feldspathic pyroxenic mica) | Tanga not Boeng | 0 | 0 | 6 | 3 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | vitric | |
| WD_33_11 | tpr315 (Tanga feldspathic pyroxenic mica) | Tanga not Boeng | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 6 | 1 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| WD_33_17 | tpr315 (Tanga feldspathic pyroxenic mica) | Tanga | 0 | 0 | 6 | 2 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | vitric | |
| WD_33_15 | tpr315 (Tanga feldspathic pyroxenic mica) | Tanga | 0 | 0 | 5 | 3 | 0 | 3 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | vitric | |
| WD_33_6 | tpr315 (Tanga feldspathic pyroxenic mica) | Tanga | 0 | 0 | 6 | 2 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | vitric | |
| WD_33_8 | tpr315 (Tanga feldspathic pyroxenic mica) | Tanga | 0 | 0 | 5 | 3 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | vitric | |
| WD_33_12 | tpr315 (Tanga feldspathic pyroxenic mica) | Tanga | 0 | 0 | 6 | 3 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | vitric | |
| WD_33_14 | tpr315 (Tanga feldspathic pyroxenic mica) | Tanga | 0 | 0 | 6 | 2 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | vitric | |
| WD_33_4 | tpr316 (Tanga feldspathic pyroxenic) | Tanga not Boeng | 0 | 0 | 5 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric | |
| WD_33_5 | tpr316 (Tanga feldspathic pyroxenic) | Tanga | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 6 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_33_3 | tpr316 (Tanga feldspathic pyroxenic) | Tanga | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric | |
| WD_54_15 | tpr335 (Navatu opaque-rich) | Viti Levu | 0 | 0 | 4 | 3 | 1 | 3 | 1 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork, microlitic, vitric, microphaneritic, plutonite | |
| WD_54_4 | tpr335 (Navatu opaque-rich) | Viti Levu | 0 | 0 | 4 | 3 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork, microlitic, vitric, microphaneritic, | |
| WD_63_22 | tpr352 (Ra pyroxenic) | Ba volcanics | 0 | 0 | 4 | 5 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric | |
| SB_2_71 | tpr371 (Nayau-Lakeba feldspathic) | Lakeba | 0 | 0 | 6 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric | |
| SB_1_75 | tpr371 (Nayau-Lakeba feldspathic) | Lakeba | 1 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, vitric | |
| SB38_1_14 | tpr371 (Nayau-Lakeba feldspathic) | Lakeba | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, vitric | |
| SB38_1_9 | tpr371 (Nayau-Lakeba feldspathic) | Lakeba | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, vitric | |
| SB38_1_48 | tpr371 (Nayau-Lakeba feldspathic) | Lakeba | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, vitric | |
| SB_5_66 | tpr371 (Nayau-Lakeba feldspathic) | Lakeba | 1 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, lathwork, vitric | |
| SB_5_100 | tpr371 (Nayau-Lakeba feldspathic) | Lakeba | 0 | 0 | 6 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric | |
| SB_6_62 | tpr371 (Nayau-Lakeba feldspathic) | Lakeba | 0 | 0 | 6 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric | |
| SB_7_89 | tpr371 (Nayau-Lakeba feldspathic) | Lakeba | 0 | 0 | 6 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, lathwork, vitric | |
| SB_6_92 | tpr371 (Nayau-Lakeba feldspathic) | Lakeba | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, vitric | |
| WD_70_10 | tpr371 (Nayau-Lakeba feldspathic) | Lau | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, vitric | |
| WD_70_11 | tpr371 (Nayau-Lakeba feldspathic) | Lau | 0 | 0 | 6 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric | |
| WD_70_12 | tpr371 (Nayau-Lakeba feldspathic) | Lau | 0 | 0 | 4 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic | |
| WD_70_8 | tpr371 (Nayau-Lakeba feldspathic) | Lau | 0 | 0 | 5 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric | |
| WD_70_9 | tpr371 (Nayau-Lakeba feldspathic) | Lau | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic | |
| WD_71_10 | tpr371 (Nayau-Lakeba feldspathic) | Lakeba | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic | |
| IL_2_2 | tpr483 (Huon feldspathic lithic) | Huon | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, plutonite, microphaneritic | |
| IL_2_20 | tpr483 (Huon feldspathic lithic) | Sio | 0 | 0 | 4 | 4 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork, microphaneritic, microlitic | |
| IL_1_18 | tpr483 (Huon feldspathic lithic) | Sio | 0 | 1 | 4 | 2 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | microphaneritic | |
| IL_1_56 | tpr483 (Huon feldspathic lithic) | Sio | 0 | 1 | 4 | 3 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, lathwork | |
| WD_67_14 | tpr365a (Mago feldspathic) | Mago | 0 | 0 | 5 | 3 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic |
Type K. Feldspathic-pyroxenic.
Nissan-11 has a full slide scan available (user: Guest pwd: Guest). 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.
Volcanic placer temper. Augite with plagioclase and hornblende.
Generally andesitic, fine- to medium-grained, subangular to subrounded temper sand of probable beach origin. Clinopyroxene dominant, but minor orthopyroxene.
Generally andesitic, fine- to medium-grained, subangular to subrounded temper sand of probable beach origin. Has orthopyroxene in addition to clinopyroxene.
Lapita sherd. Pyroxenes are 1/3 orthopyroxene.
Lapita sherd. Pyroxenes are 1/3 orthopyroxene.
Pyroxenes are 1/3 orthopyroxene
Pyroxenes are 1/3 orthopyroxene
Lapita sherd. Pyroxenes are 1/3 orthopyroxene.
Lapita sherd. Pyroxenes are 1/3 orthopyroxene.
Vitric.
Tan vitric.
Tan vitric.
Tan vitric. Retoka.
Vitric.
Vitric.
Vitric.
Vitric.
Vitric.
Vitric.
Vitric.
Vitric.
Probably from Mele Plain.
Probably from Mele Plain.
Feldspathic standard Efate.
Feldspathic standard Efate.
Feldspathic standard Efate.
Feldspathic standard Efate.
Feldspathic standard Efate.
Probably from Mele Plain.
Vitric.
Vitric.
Pale (felsic) vitric, may be from Efate.
Found Tongoa (Shepherd Islands). Tan vitric.
Tan pumiceous vitrics.
Tan pumiceous vitrics
Tan pumiceous vitrics.
Temper sand mainly composed of plagioclase and clinopyroxene grains, but with subordinate proportions of Yap metavolcanics.
Temper sand mainly composed of plagioclase and clinopyroxene grains, but with subordinate proportions of Yap metavolcanics.
Grog (composed of broken pottery).
Lifafaesing site. Feldspathic temper sand that contains abundant clinopyroxene and sparse mica.
Matambek site. Feldspathic temper sand that contains abundant clinopyroxene and sparse mica.
Angkikita site. Feldspathic temper sand that contains abundant clinopyroxene and biotite.
Matangkipit. Feldspathic temper sand that contains abundant clinopyroxene and sparse mica.
Amfuli site. Feldspathic temper sand that contains abundant clinopyroxene and sparse mica.
Amfuli. Feldspathic temper sand that contains abundant clinopyroxene and sparse mica.
Salkangkis. Feldspathic temper sand that contains abundant clinopyroxene and sparse mica.
Baba. Feldspathic temper sand that contains abundant clinopyroxene and sparse mica.
Ansingsing. Feldspathic temper sand that contains abundant clinopyroxene and sparse mica.
Matambek site. Feldspathic temper sand that contains abundant clinopyroxene no biotite.
Angkikita site. Feldspathic temper sand that contains abundant clinopyroxene and no biotite.
Nonu site. Feldspathic temper sand that contains abundant clinopyroxene no biotite.
Opaque placer.
Opaque rich.
Lapita sherd. Low hornblendes, from Ba volcanics.
Feldspathic.
Feldspathic.
Feldspathic
Feldspathic.
Feldspathic
Oil-lamp. Feldspathic, with some calcareous.
Applique. Feldspathic.
Dari (flared-rim bowl). Feldspathic.
Saqa (oil/water jar). Feldspathic.
Feldspathic, but towards feldspathic-lithic.
Volcanic rock (lithic) fragments, where vitric are tan to red glassy grains, and microlitic grains include both hyalopilitic (plagioclase microlites set in clear brown volcanic glass) and tachylitic (plagioclase microlites set in opaque volcanic glass) grains .
Volcanic rock (lithic) fragments, where vitric are tan to red glassy grains, and microlitic grains include both hyalopilitic (plagioclase microlites set in clear brown volcanic glass) and tachylitic (plagioclase microlites set in opaque volcanic glass) grains.
Volcanic rock (lithic) fragments, where vitric are tan to red glassy grains, and microlitic grains include both hyalopilitic (plagioclase microlites set in clear brown volcanic glass) and tachylitic (plagioclase microlites set in opaque volcanic glass) grains.
Volcanic rock (lithic) fragments, where vitric are tan to red glassy grains, and microlitic grains include both hyalopilitic (plagioclase microlites set in clear brown volcanic glass) and tachylitic (plagioclase microlites set in opaque volcanic glass) grains.
Volcanic rock (lithic) fragments, where vitric are tan to red glassy grains, and microlitic grains include both hyalopilitic (plagioclase microlites set in clear brown volcanic glass) and tachylitic (plagioclase microlites set in opaque volcanic glass) grains.
Feldspathic. Imported.
Sio style. CAUTION: Section less than 30microns. in diameter. Volcanic rock fragments (<10%) are up to 0.5 rnn across and contain feldspar microlites, opaques and altered glass. Angular pyroxene crystals are accessory. Elongate and rounded pellets are devoid of inclusions. The sherd also contains some large (up to 2 nm in length) ferruginized fragments which also contain opaques and plagioclase. These may be broken pot fragments. Opaque minerals.
Sio style. CAUTION: Section less than 30microns. Pyroxene grains (5%) are generally less than 0.4 m in length. Plagioclase laths (5%) are less than 0.2 mm in length. There are some large volcanic rock fragments made up of abundant plagioclase laths, minor pyroxene and fine grained opaques in a hypocrystallne texture. Accessory iron oxide and red ferruginized clay pellets are also present. The clay is dark brown.
Sio style. CAUTION: Section less than 30microns. This dark red to black sherd contains abundant quartz and plagioclase up to 0.1 mm in length. There are some large pyroxene and volcanic rock fragments up to 0.4 mm in length but these grains are only accessory.
Pyroxene grains (10%).Quartz and feldspar grains (<10%). There are some hypocrystalline volcanic rock fragments which contain large pyroxene crystals set in a ground mass of smaller pyroxene crystals, plagioclase, opaques and altered glass. The sherd also contains trace amounts of iron oxide and carbonate shell fragments.
Non-placer indigenous temper.
Early Mussau Lapita (3250 - 2950 BP)
Post Lapita Buka (2200 - 0 BP)
Late Far Western Lapita (2980 - 1800 BP)
Early Far Western Lapita (3500 - 2770 BP)
Middle Far Western Lapita (3050 - 2300 BP)
Early Mangaasi (2200 - 1600 BP)
Late Mangaasi (1600 - 1200 BP)
Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP)
Palau grog ware (2500 - 200 BP)
Transitional Far Western (2350 - 1900 BP)
Futuna Polynesian Plainware (2100 - 1700 BP)