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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 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| tpr200 ** | 6 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | limeclast |
| Telepunu calcareous | 6 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Maluku |
| tpr202 ** | 3 | 3 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 6 | 0 | quartzite, tectonite |
| Buru hybrid | 2 | 3 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | Maluku |
| tpr199 ** | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| Raca calcareous | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Maluku |
| tpr201 ** | 4 | 3 | 2 | 1 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 2 | 4 | 0 | argillitic, siltstone, chert |
| Vasino hybrid | 2 | 2 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 4 | 0 | Maluku |
| tpr203 ** | 0 | 0 | 5 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic |
| Banda pyroxenic-feldspathic | 0 | 0 | 3 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Maluku |
| 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_86_10 | tpr200 (Telepunu calcareous) | Timor | puhu (Historic Timor) (1500 - 0 BP) | 6 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | limeclast |
| WD_86_11 | tpr202 (Buru hybrid) | Buru | Early Metal Age Maluku Tengah (2300 - 1000 BP) | 2 | 3 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | quartzite, tectonite |
| WD_85_1 | tpr199 (Raca calcareous) | Timor | puhu (Historic Timor) (1500 - 0 BP) | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| WD_85_8 | tpr199 (Raca calcareous) | Timor | puhu (Historic Timor) (1500 - 0 BP) | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| WD_85_10 | tpr200 (Telepunu calcareous) | Timor | puhu (Historic Timor) (1500 - 0 BP) | 6 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | limeclast |
| WD_85_11 | tpr201 (Vasino hybrid) | Timor | puhu (Historic Timor) (1500 - 0 BP) | 3 | 3 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 4 | 0 | argillitic, siltstone, chert |
| WD_85_7 | tpr202 (Buru hybrid) | Buru | Early Metal Age Maluku Tengah (2300 - 1000 BP) | 3 | 3 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | quartzite, tectonite |
| WD_85_6 | tpr202 (Buru hybrid) | Buru | Early Metal Age Maluku Tengah (2300 - 1000 BP) | 3 | 3 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | quartzite, tectonite |
| WD_85_15 | tpr203 (Banda pyroxenic-feldspathic) | Banda | puhu (Historic Timor) (1500 - 0 BP) | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic |
| WD_86_5 | tpr200 (Telepunu calcareous) | Timor | Early Metal Age Timor (2300 - 1500 BP) | 6 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | limeclast |
| WD_86_6 | tpr200 (Telepunu calcareous) | Timor | Early Metal Age Timor (2300 - 1500 BP) | 6 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | limeclast |
| WD_86_1 | tpr199 (Raca calcareous) | Timor | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na | |
| WD_86_2 | tpr199 (Raca calcareous) | Timor | puhu (Historic Timor) (1500 - 0 BP) | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| WD_86_12 | tpr199 (Raca calcareous) | Timor | puhu (Historic Timor) (1500 - 0 BP) | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| WD_86_13 | tpr200 (Telepunu calcareous) | Timor | puhu (Historic Timor) (1500 - 0 BP) | 6 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | limeclast |
| WD_86_14 | tpr200 (Telepunu calcareous) | Timor | puhu (Historic Timor) (1500 - 0 BP) | 6 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | limeclast |
| WD_86_15 | tpr201 (Vasino hybrid) | Timor | puhu (Historic Timor) (1500 - 0 BP) | 3 | 3 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 4 | 0 | argillitic, siltstone, chert |
| WD_86_17 | tpr201 (Vasino hybrid) | Timor | puhu (Historic Timor) (1500 - 0 BP) | 2 | 3 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 4 | 0 | argillitic, siltstone, chert |
Hybrid sand composed predominantly of calcareous limeclasts made of diagenetic microspar, with which subordinate terrigenous grains of quartz and feldspar. Derived from the erosion of indurated limestone on Timor.
Hybrid coastal sand (metamorphic terrigenous detritus). Moderately to well sorted, subrounded hybrid (mixed calcareous and terrigenous aggregate) temper sands of presumed beach origin in which terrigenous grains were derived from foliated metasedimentary bedrock.
Raca-type temper (foraminiferal calcareous grains).
Raca-type temper (foraminiferal calcareous grains).
Telepunu-type temper (limeclast calcareous grains).
Lithic-type. Also called MA_C7_1562.
M64 has a full slide scan available (user: Guest pwd: Guest). Imaged by K. Hardy and M. Leclerc, ANU.
Hybrid coastal sand (metamorphic terrigenous detritus). Moderately to well sorted, subrounded hybrid (mixed calcareous and terrigenous aggregate) temper sands of presumed beach origin in which terrigenous grains were derived from foliated metasedimentary bedrock.
Hybrid coastal sand (metamorphic terrigenous detritus). Moderately to well sorted, subrounded hybrid (mixed calcareous and terrigenous aggregate) temper sands of presumed beach origin in which terrigenous grains were derived from foliated metasedimentary bedrock.
Plagioclase-rich volcanic sand temper. Volcanic glass shards of vitroclastic texture.
TP2-3 has a full slide scan available (user: Guest pwd: Guest). Imaged by K. Hardy and M. Leclerc, ANU.
Sand temper made up predominantly of subrounded to rounded calcareous grains.
Hybrid sand composed predominantly of calcareous limeclasts made of diagenetic microspar, with which subordinate terrigenous grains of quartz and feldspar. Derived from the erosion of indurated limestone on Timor.
Almost exclusively calcareous temper sand composed predominantly of rather evenly sized and globular foraminiferal tests that are hollow.
Almost exclusively calcareous temper sand composed predominantly of rather evenly sized and globular foraminiferal tests that are hollow.
Raca-type temper (foraminiferal calcareous grains).
Mixed Raca-Telepunu type temper (both limeclast and foraminiferal calcareous grains).
Telepunu-type temper (limeclast calcareous grains).
VA-A4-57 has a full slide scan available (user: Guest pwd: Guest). Imaged by K. Hardy and M. Leclerc, ANU.
Vasino-type temper (hybrid lithic Timor sands).
Lithic hybrid sand in which lithic terrigenous detritus is admixed in variable proportions with calcareous grains that include both massive grains and foraminiferal tests. Lithic fragments of sedimentary rock- dominantly murky argillite (or shale or mudstone).