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 |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
tpr134 | 1 | 0 | 2 | 5 | 1 | 4 | 2 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
TLTF olivine placer | 0 | 0 | 0 | 4 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
tpr178 | 0 | 1 | 4 | 3 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic |
Bismarck pyroxenic | 0 | 0 | 3 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Bismarck |
tpr179 | 0 | 0 | 5 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | felsitic |
Bismarck feldspathic | 0 | 0 | 5 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Bismarck |
tpr180 | 0 | 0 | 2 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, microlitic |
Bismarck lithic | 0 | 0 | 2 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Bismarck |
Slide | Fabric | Possible Origin | Cal. | Quartz | Feldspar | Pyroxene | Amphibole | Opaques | Olivine | Biotite | Muscovite | Epidote | Garnet/ Spinel | Ig./Met. Rocks | Sed. Rocks | Grog | Lithics |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
WD_102_1 | tpr134 (TLTF olivine placer) | TLTF or New Britain | 0 | 0 | 2 | 5 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
WD_102_2 | tpr178 (Bismarck pyroxenic) | Anir | 0 | 1 | 3 | 2 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic |
WD_102_4 | tpr178 (Bismarck pyroxenic) | Anir | 0 | 0 | 4 | 3 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic |
WD_102_3 | tpr179 (Bismarck feldspathic) | Anir | 0 | 0 | 5 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | felsitic |
WD_102_5 | tpr180 (Bismarck lithic) | Anir | 0 | 0 | 2 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, microlitic |
Non-Lapita. Well sorted, subrounded to subangular aggreates that are probably beach sands Olivine and hornblende present. Has orthopyroxene in addition to the more abundant clinopyroxene. Microlitics are hyalopilitic.
Non-Lapita. Moderately sorted, subangular to subrounded aggregates, probably stream sands. Microlitic volcanic rock fragments are hyalopilitic.
Non-Lapita. Moderately sorted, subangular to subrounded aggregates, probably stream sands. Microlitic lithics are hyalopilitic.
Non-Lapita. Well sorted, subrounded to subangular aggreates that are probably beach sands. Volcanic rocks are felsitic (microcrystalline quartz-feldspar groundmass mosaic commonly with plagioclase microphenocrysts).
Non-Lapita. Vitric glass. Well sorted, subrounded to subangular aggreates that are probably beach sands. Microlitic lithics are hyalopilitic.