| 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 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| tpr213 | 1 | 0 | 5 | 6 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric, felsitic |
| Santo beach | 0 | 0 | 1 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Vanuatu |
| tpr214 | 1 | 0 | 5 | 4 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, vitric, felsitic |
| Santo stream | 0 | 0 | 2 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Vanuatu |
| tpr215 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| Anomalous Santo vitric | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Vanuatu |
| tpr216a | 0 | 6 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | quartzite |
| Exotic Santo quartzose | 0 | 6 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | Vanuatu |
| tpr219 | 0 | 0 | 3 | 3 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, vitric, felsitic |
| Santo-Malo lithic | 0 | 0 | 2 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | Vanuatu |
| Slide | Fabric | Possible Origin | Cal. | Quartz | Feldspar | Pyroxene | Amphibole | Opaques | Olivine | Biotite | Muscovite | Epidote | Garnet/ Spinel | Ig./Met. Rocks | Sed. Rocks | Grog | Lithics |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| WD_57_12 | tpr213 (Santo beach) | Santo | 1 | 0 | 5 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| WD_57_17 | tpr213 (Santo beach) | Santo | 0 | 0 | 1 | 6 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric |
| WD_57_13 | tpr214 (Santo stream) | Santo | 1 | 0 | 3 | 4 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| WD_57_23 | tpr214 (Santo stream) | Santo | 0 | 0 | 3 | 4 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, vitric |
| WD_57_24 | tpr214 (Santo stream) | Santo | 0 | 0 | 5 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, vitric |
| WD_57_16 | tpr215 (Anomalous Santo vitric) | Vanuatu | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| WD_57_22 | tpr216a (Exotic Santo quartzose) | New Caledonia | 0 | 6 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | quartzite |
| WD_51_3 | tpr219 (Santo-Malo lithic) | Santo | 0 | 0 | 3 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, vitric |
Sand temper in which plagioclase and clinopyroxene mineral grains and lithic fragments of microlitic to vitric andesitic rock are the prominent grain types. some clasts are skeletal calcareous grains of modern reef derivation (well sorted and subrounded).
Sand temper in which plagioclase and clinopyroxene mineral grains and lithic fragments of microlitic to vitric andesitic rock are the prominent grain types. Clinopyroxene dominant, but minor orthopyroxene.
Sand temper in which plagioclase and clinopyroxene mineral grains and lithic fragments of microlitic to vitric andesitic rock are the prominent grain types. Moderately to poorly sorted and subangular.
Sand temper in which plagioclase and clinopyroxene mineral grains and lithic fragments of microlitic to vitric andesitic rock are the prominent grain types. (moderately to poorly sorted and subangular).
Sand temper in which plagioclase and clinopyroxene mineral grains and lithic fragments of microlitic to vitric andesitic rock are the prominent grain types. (moderately to poorly sorted and subangular).
Two kinds of volcanic glass, one being dark brown mafic volcanic glass, and the other being pale tan to colorless felsic volcanic glass.
High quartz.
Lithic. Modern Santo sherd.