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Many fabrics have a range of abundances. The range maximum (top) and minimum (bottom) are shown.
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| 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 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| tpr216 ** | 1 | 2 | 2 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 3 | 3 | 1 | 0 | quartzite, plutonite, metavolcanic |
| Exotic Malo chrome spinel | 1 | 2 | 2 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 3 | 3 | 1 | 0 | Vanuatu |
| tpr217 | 0 | 0 | 4 | 3 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, vitric, felsitic |
| Malo feldspathic | 0 | 0 | 4 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Vanuatu |
| tpr218 | 0 | 0 | 3 | 5 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric, felsitic |
| Malo pyroxenic | 0 | 0 | 2 | 4 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 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 |
| 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 |
| 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_21 | tpr216 (Exotic Malo chrome spinel) | New Caledonia | 1 | 2 | 2 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 3 | 3 | 1 | 0 | quartzite, plutonite, metavolcanic |
| WD_51_16 | tpr217 (Malo feldspathic) | Santo | 0 | 0 | 4 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| WD_51_17 | tpr217 (Malo feldspathic) | Santo | 0 | 0 | 4 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| WD_51_18 | tpr217 (Malo feldspathic) | Santo | 0 | 0 | 4 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| WD_51_14 | tpr218 (Malo pyroxenic) | Santo | 0 | 0 | 3 | 5 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric |
| WD_51_15 | tpr218 (Malo pyroxenic) | Santo | 0 | 0 | 2 | 5 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| WD_51_4 | tpr219 (Santo-Malo lithic) | Santo | 0 | 0 | 2 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, vitric |
| WD_51_6 | tpr219 (Santo-Malo lithic) | Santo | 0 | 0 | 2 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, vitric |
| WD_51_8 | tpr219 (Santo-Malo lithic) | Santo | 0 | 0 | 2 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, vitric |
| 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 |
| ML_1_11 | tpr214 (Santo stream) | Santo | 0 | 0 | 5 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, microlitic, vitric |
| ML_1_12 | tpr214 (Santo stream) | Santo | 0 | 0 | 4 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, felsitic, vitric |
| ML_1_13 | tpr214 (Santo stream) | Santo | 0 | 0 | 3 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, microlitic |
Chrome spinel, orthopyroxene, and serpentinite grains are characteristic of ultramafic detritus.
Dominantly plagioclase, some pyroxene, partly crystalline volcanic rock fragments, some volcanic glass.
Feldspar rich.
Dominantly plagioclase, some pyroxene, partly crystalline volcanic rock fragments, some volcanic glass, some calcareous.
Pyroxene rich with opaque iron oxides.
Pyroxene rich with opaque iron oxides.
Volcanic rock fragments- poorly sorted alluvial sand, microlitic with dark vitric.
Volcanic rock fragments- poorly sorted alluvial sand, microlitic with dark vitric.
Volcanic rock fragments- poorly sorted alluvial sand, microlitic with dark 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.
Plagioclase-rich, felsitic.
Clinopyroxene-rich.
Clinopyroxene-rich. Modern sherd.