| 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 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| tpr76 | 4 | 2 | 2 | 1 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 4 | 0 | 0 | vitric |
| Ambon hybrid | 4 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Maluku |
| tpr78 | 0 | 3 | 3 | 1 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| Ambon-Haruku rhyolite | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Maluku |
| tpr80 | 0 | 6 | 2 | 1 | 1 | 0 | 0 | 3 | 1 | 0 | 0 | 0 | 3 | 0 | quartzite, tectonite |
| Gorom-Seram quartzose | 0 | 4 | 1 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 2 | 0 | Maluku |
| Slide | Fabric | Possible Origin | Cal. | Quartz | Feldspar | Pyroxene | Amphibole | Opaques | Olivine | Biotite | Muscovite | Epidote | Garnet/ Spinel | Ig./Met. Rocks | Sed. Rocks | Grog | Lithics |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| WD_19_10 | tpr76 (Ambon hybrid) | Ambon | 4 | 2 | 1 | 1 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 4 | 0 | 0 | vitric |
| WD_19_11 | tpr76 (Ambon hybrid) | Ambon | 4 | 2 | 1 | 1 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 4 | 0 | 0 | vitric |
| WD_19_6 | tpr76 (Ambon hybrid) | Ambon | 4 | 2 | 1 | 1 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 4 | 0 | 0 | vitric |
| WD_19_13 | tpr78 (Ambon-Haruku rhyolite) | Ambon | 0 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| WD_20_12 | tpr78 (Ambon-Haruku rhyolite) | Ambon/Haruku | 0 | 3 | 3 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric |
| WD_20_13 | tpr78 (Ambon-Haruku rhyolite) | Ambon/Haruku | 0 | 3 | 3 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 5 | 0 | 0 | vitric |
| WD_19_4 | tpr78 (Ambon-Haruku rhyolite) | Haruku | 0 | 2 | 2 | 1 | 1 | 2 | 0 | 1 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| WD_20_11 | tpr78 (Ambon-Haruku rhyolite) | Ambon/Haruku | 0 | 2 | 2 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| WD_20_7 | tpr80 (Gorom-Seram quartzose) | Seram | 0 | 4 | 2 | 1 | 1 | 0 | 0 | 3 | 1 | 0 | 0 | 0 | 2 | 0 | quartzite, tectonite |
| WD_20_5 | tpr80 (Gorom-Seram quartzose) | Seram | 0 | 4 | 2 | 1 | 1 | 0 | 0 | 3 | 1 | 0 | 0 | 0 | 2 | 0 | quartzite, tectonite |
Modern sherd. Pale glass (felsic) predominates over brown.
Modern sherd. Pale glass (felsic) predominates over brown.
Local sand.
Stream sand.
Ambon indi or exotic (Haruku). Prehistoric sherd. Rhyolitic temper sand characteristic of Haruku origin. Pale glass (felsic) predominates over brown.
Ambon indi or exotic (Haruku). Prehistoric sherd. Rhyolitic temper sand characteristic of Haruku origin. Pale glass (felsic) predominates over brown.
Modern sherd. Rhyolite. Pale glass (felsic) predominates over brown.
Ambon indi or exotic (Haruku). Prehistoric sherd. Rhyolitic temper sand characteristic of Haruku origin. Pale glass (felsic) predominates over brown.
HT1-2 has a full slide scan available (user: Guest pwd: Guest). Imaged by K. Hardy and M. Leclerc, ANU.
Imported from Seram. Prehistoric sherd. Mineralogically complex non-volcanic sand temper. Quartz, feldspar, chert-argillite, mica, tectonite, amphibole, clinopyroxene, serpentinite.
Prehistoric sherd. Mineralogically complex non-volcanic sand temper. Exotic Ambon (Seram). Quartz, feldspar, chert-argillite, mica, tectonite, amphibole, clinopyroxene, serpentinite.