Feldspathic (Q137397286)
Dominated by feldspar inclusions.
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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 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| tpr198 | 0 | 0 | 6 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| Watom feldspathic | 0 | 0 | 6 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Bismarck |
| tpr101 | 0 | 0 | 6 | 1 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic, felsitic |
| New Ireland feldspathic non-placer | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr296b ** | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| New Caledonian feldspathic | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | New Caledonia |
| tpr418 | 0 | 1 | 6 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | vitric |
| Ryukyu feldspathic | 0 | 1 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Japan |
| tpr308 | 0 | 2 | 6 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | microlitic, serpentinite, chert |
| New Caledonian plagiogranite | 0 | 2 | 6 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | New Caledonia |
| tpr191b | 0 | 3 | 4 | 1 | 2 | 2 | 0 | 1 | 0 | 0 | 0 | 4 | 0 | 0 | felsitic, vitric, microlitic |
| Admiralty Feldspathic Felsitic | 0 | 2 | 4 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr178a | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic |
| TLTF feldspathic | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Bismarck |
| 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_31_1 | tpr101 (New Ireland feldspathic non-placer) | New Ireland | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic, felsitic |
| WD_104_1 | tpr198 (Watom feldspathic) | New Britain-Solomons | Middle Far Western Lapita (3050 - 2300 BP) | 0 | 0 | 6 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic, vitric, microlitic |
| WD_104_17 | tpr198 (Watom feldspathic) | New Britain-Solomons | Middle Far Western Lapita (3050 - 2300 BP) | 0 | 0 | 6 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic, vitric, microlitic |
| WD_96_11 | tpr418 (Ryukyu feldspathic) | Ryukyu | 0 | 1 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | na | |
| WD_96_12 | tpr418 (Ryukyu feldspathic) | Ryukyu | 0 | 1 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | na | |
| WD_96_13 | tpr418 (Ryukyu feldspathic) | Ryukyu | 0 | 1 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | na | |
| WD_96_15 | tpr418 (Ryukyu feldspathic) | Ryukyu | 0 | 1 | 6 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric | |
| WD_96_16 | tpr418 (Ryukyu feldspathic) | Ryukyu | 0 | 1 | 6 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric | |
| WD_27_10 | tpr296b (New Caledonian feldspathic) | New Caledonia | Southern Lapita (3050 - 2750 BP) | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
Feldspathic non-placer sand temper.
Plagioclase high.
Plagioclase high.
Feldspathic temper, with maybe some grog.
Feldspathic with perhaps grog.
Feldspathic temper with maybe grog.
Feldspathic temper.
Feldspathic.
Lapita sherd. Plagioclase dominates, very weathered.
Transitional Far Western (2350 - 1900 BP)
Middle Far Western Lapita (3050 - 2300 BP)
Late Far Western Lapita (2980 - 1800 BP)