Backarc Quartzose (Q137391967)
Clinopyroxenes, plagioclase, and lithics of basalts or shoshonite (a basaltic trachyandesite), dominate with quartz.
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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 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| tpr94 ** | 6 | 1 | 1 | 2 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, felsitic, vitric |
| Mussau type CD | 0 | 0 | 1 | 1 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Bismarck |
| tpr106 | 4 | 3 | 2 | 1 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na |
| Exotic New Ireland quartz-calcite | 4 | 3 | 2 | 1 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr93 ** | 6 | 1 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | felsitic, vitric, chert |
| Mussau type B | 6 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Bismarck |
| tpr191b | 0 | 3 | 4 | 1 | 2 | 2 | 0 | 1 | 0 | 0 | 0 | 4 | 0 | 0 | felsitic, vitric, microlitic |
| Admiralty Feldspathic Felsitic | 0 | 2 | 4 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| Slide | Fabric | Possible Origin | Ware | Cal. | Quartz | Feldspar | Pyroxene | Amphibole | Opaques | Olivine | Biotite | Muscovite | Epidote | Garnet/ Spinel | Ig./Met. Rocks | Sed. Rocks | Grog | Lithics |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| WD_31_14 | tpr106 (Exotic New Ireland quartz-calcite) | Admiralty | Middle Far Western Lapita (3050 - 2300 BP) | 4 | 3 | 2 | 1 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na |
| WD_36_17 | tpr93 (Mussau type B) | Admiralty | Early Mussau Lapita (3250 - 2950 BP) | 6 | 1 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | felsitic, vitric, chert |
| WD_36_20 | tpr93 (Mussau type B) | Admiralty | Early Mussau Lapita (3250 - 2950 BP) | 6 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic, vitric |
| WD_36_24 | tpr93 (Mussau type B) | Admiralty | Early Mussau Lapita (3250 - 2950 BP) | 6 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | felsitic, vitric, chert |
| WD_37_2 | tpr94 (Mussau type CD) | Admiralty | Early Mussau Lapita (3250 - 2950 BP) | 0 | 1 | 2 | 1 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic, vitric |
| WD_37_6 | tpr94 (Mussau type CD) | Admiralty | Late Mussau Lapita (2950 - 2700 BP) | 3 | 1 | 1 | 1 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic, vitric |
Hybrid (mixed terrigenous-calcareous) beach sand temper of anomalous composition unlikely to derive from anywhere on New Ireland or within the Bismarck Archipelago.
Calcareous marginally hybrid (Type B).
Calcareous marginally hybrid (Type B).
Calcareous marginally hybrid (Type B).
Opaque rich placer sands (Type CD).
Opaque rich placer sands (Type CD).
Late Far Western Lapita (2980 - 1800 BP)
Transitional Far Western (2350 - 1900 BP)
Middle Far Western Lapita (3050 - 2300 BP)