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 |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Max | 0 | 1 | 4 | 2 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 5 | 0 | 0 | microphaneritic, microlitic |
Min | 0 | 0 | 3 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Solomons |
Slide | Site | Possible Origin | Cal. | Quartz | Feldspar | Pyroxene | Amphibole | Opaques | Olivine | Biotite | Muscovite | Epidote | Garnet/ Spinel | Ig./Met. Rocks | Sed. Rocks | Grog | Lithics |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
WD_101_3 | Buka (Buka) | Buka | 0 | 0 | 4 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microphaneritic, microlitic |
WD_101_6 | Ontong Java Atoll (Ontong Java Atoll) | Buka | 0 | 0 | 4 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microphaneritic, microlitic |
WD_101_7 | Ontong Java Atoll (Ontong Java Atoll) | Buka | 0 | 0 | 3 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microphaneritic |
WD_32_13 | Nissan (Nissan) | Buka | 0 | 0 | 3 | 2 | 2 | 2 | 0 | 1 | 0 | 0 | 0 | 5 | 0 | 0 | microphaneritic, microlitic |
WD_32_20 | Nissan (Nissan) | Buka | 0 | 0 | 4 | 2 | 1 | 2 | 0 | 1 | 0 | 0 | 0 | 5 | 0 | 0 | microphaneritic, microlitic |
WD_32_25 | Nissan (Nissan) | Buka | 0 | 0 | 5 | 2 | 1 | 2 | 0 | 2 | 0 | 0 | 0 | 4 | 0 | 0 | microphaneritic, microlitic |
WD_35_19 | Ontong Java Atoll (Ontong Java Atoll) | Buka | 0 | 0 | 4 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microphaneritic |
WD_35_20 | Ontong Java Atoll (Ontong Java Atoll) | Buka | 0 | 0 | 3 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microphaneritic |
Non-Lapita. Poorly sorted and weathered volcanic sand. Plagioclase and microphaneritic igneous rock fragments (microgranular grains composed dominantly of plagioclase-clinopyroxene with subophitic internal texture of clinopyroxene crystals partly enclosing plagioclase laths), microlitic volcanic rock fragments, opaque iron oxides, clinopyroxene, green hornblende, and deeply weathered brown biotite
Microgranular temper. May not be from Buka- has different hornblende:pyroxene ratio.
Microgranular temper. May not be from Buka- has different hornblende:pyroxene ratio.
Buka wares Fine-grained microgranular rock fragments dominant.
Buka wares Fine-grained microgranular rock fragments dominant.
Poorly sorted temper sand characteristic of Buka temper types.
Microgranular temper. May not be from Buka- has different hornblende:pyroxene ratio.
Microgranular temper. May not be from Buka- has different hornblende:pyroxene ratio.