Lathwork (Q137423761)
Dominated by lathwork 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 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| tpr462 ** | 4 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, microlitic |
| Exotic Tuam lithic | 4 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | PNG |
| tpr294c ** | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| Samoan basaltic lithic C | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Samoa |
| tpr294d ** | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| Samoan basaltic lithic D | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Samoa |
| tpr289 ** | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, vitric |
| Savaii basaltic | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Samoa |
| tpr328 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, vitric |
| Uvea basaltic lithic | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | NE Melanesia |
| tpr294a ** | 0 | 0 | 1 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| Samoan basaltic lithic A | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Samoa |
| Slide | Fabric | Possible Origin | Cal. | Quartz | Feldspar | Pyroxene | Amphibole | Opaques | Olivine | Biotite | Muscovite | Epidote | Garnet/ Spinel | Ig./Met. Rocks | Sed. Rocks | Grog | Lithics |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| WD_25_20 | tpr289 (Savaii basaltic) | Samoa | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| WD_79_1 | tpr294a (Samoan basaltic lithic A) | Olomoana Mountain Tutuila | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_79_6 | tpr294a (Samoan basaltic lithic A) | Olomoana Mountain Tutuila | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_87_24 | tpr294a (Samoan basaltic lithic A) | Olomoana Mountain Tutuila | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_87_10 | tpr294a (Samoan basaltic lithic A) | Olomoana Mountain Tutuila | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| WD_87_3 | tpr294a (Samoan basaltic lithic A) | Olomoana Mountain Tutuila | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_87_12 | tpr294a (Samoan basaltic lithic A) | Olomoana Mountain Tutuila | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_87_16 | tpr294a (Samoan basaltic lithic A) | Olomoana Mountain Tutuila | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_87_17 | tpr294a (Samoan basaltic lithic A) | Olomoana Mountain Tutuila | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_87_18 | tpr294a (Samoan basaltic lithic A) | Olomoana Mountain Tutuila | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_87_4 | tpr294a (Samoan basaltic lithic A) | Olomoana Mountain Tutuila | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_79_15 | tpr294c (Samoan basaltic lithic C) | Olomoana Mountain Tutuila | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_79_16 | tpr294c (Samoan basaltic lithic C) | Olomoana Mountain Tutuila | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| WD_79_17 | tpr294c (Samoan basaltic lithic C) | Olomoana Mountain Tutuila | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| WD_79_19 | tpr294d (Samoan basaltic lithic D) | Olomoana Mountain Tutuila | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| WD_79_20 | tpr294d (Samoan basaltic lithic D) | Olomoana Mountain Tutuila | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| IL_2_5 | tpr462 (Exotic Tuam lithic) | ? | 4 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, microlitic |
Basaltic rock.
Intersertal with tachylitic glass and subordinate hyalopilitic. A3.
Intersertal to intergranular with minor hyalopilitic.
Intersertal with tachylitic glass and subordinate hyalopilitic. A3.
Intersertal to intergranular with minor hyalopilitic.
Intersertal to intergranular with minor hyalopilitic.
Intersertal to intergranular with minor hyalopilitic.
Intersertal to intergranular with minor hyalopilitic.
Intersertal to intergranular with minor hyalopilitic.
Intersertal to intergranular with minor hyalopilitic.
Intersertal to intergranular with minor hyalopilitic.
Intergranular with minor hyalopilitic
Intergranular with minor hyalopilitic.
Intergranular with minor hyalopilitic
Subophitic with minor hyalopilitic.
Subophitic with minor hyalopilitic.
Lapita style. The pale brown clay contains remnant shelly fragments, up to 0.3 mm in length. Volcanic rock fragments contain mainly plagioclase crystals and tiny feldspar grains up to 0.5 mm in length. Subrounded ferruginized clasts and angular feldspar grains are about 0.2 mm in length. Contains wavy layers of red brown clay.