Cagua: Andesite / Basaltic Andesite, Composite type, Stratovolcano.
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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 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| tpr55 | 0 | 1 | 6 | 1 | 3 | 2 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | microlitic, felsitic, vitric, microphaneritic |
| Cagayan feldspathic | 0 | 1 | 5 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Philippines |
| tpr56 | 0 | 1 | 4 | 2 | 3 | 2 | 0 | 1 | 0 | 1 | 0 | 4 | 0 | 0 | microlitic, microphaneritic, vitric, felsitic |
| Cagayan lithic | 0 | 1 | 4 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 1 | 0 | Philippines |
| tpr57 ** | 0 | 1 | 3 | 3 | 1 | 3 | 1 | 0 | 0 | 0 | 0 | 5 | 3 | 0 | vitric, microlitic, microphaneritic, argillitic, chert |
| Luzon tectonic highland | 0 | 0 | 1 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 1 | 0 | Philippines |
| 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_15_6a | tpr55 (Cagayan feldspathic) | 0 | 1 | 5 | 1 | 2 | 2 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | microlitic, felsitic, vitric | ||
| WD_15_7a | tpr55 (Cagayan feldspathic) | 0 | 1 | 5 | 1 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, vitric, microphaneritic | ||
| WD_15_7b | tpr55 (Cagayan feldspathic) | 0 | 1 | 5 | 1 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, vitric, microphaneritic | ||
| WD_15_10a | tpr56 (Cagayan lithic) | 0 | 1 | 4 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, microphaneritic, vitric, felsitic | ||
| WD_15_10b | tpr56 (Cagayan lithic) | 0 | 1 | 4 | 1 | 2 | 2 | 0 | 1 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, microphaneritic, vitric, felsitic | ||
| WD_15_10c | tpr56 (Cagayan lithic) | 0 | 1 | 4 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, microphaneritic, vitric, felsitic | ||
| WD_15_5a | tpr55 (Cagayan feldspathic) | 0 | 1 | 6 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, vitric | ||
| WD_15_5b | tpr55 (Cagayan feldspathic) | 0 | 1 | 6 | 0 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, felsitic, vitric | ||
| WD_15_5c | tpr55 (Cagayan feldspathic) | 0 | 1 | 6 | 0 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, vitric | ||
| WD_15_6aa | tpr55 (Cagayan feldspathic) | 0 | 1 | 5 | 2 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, vitric | ||
| WD_15_6b | tpr55 (Cagayan feldspathic) | 0 | 1 | 6 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, felsitic, vitric | ||
| WD_15_6bb | tpr56 (Cagayan lithic) | 0 | 1 | 4 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, microphaneritic, vitric, felsitic | ||
| WD_15_9a | tpr56 (Cagayan lithic) | 0 | 1 | 4 | 1 | 3 | 2 | 0 | 0 | 0 | 1 | 0 | 4 | 0 | 0 | microlitic, microphaneritic, vitric, felsitic | ||
| WD_15_9b | tpr56 (Cagayan lithic) | 0 | 1 | 4 | 1 | 2 | 2 | 0 | 0 | 0 | 1 | 0 | 4 | 0 | 0 | microlitic, microphaneritic, vitric, felsitic | ||
| WD_15_9c | tpr56 (Cagayan lithic) | 0 | 1 | 4 | 1 | 2 | 2 | 0 | 0 | 0 | 1 | 0 | 4 | 0 | 0 | microlitic, microphaneritic, vitric, felsitic | ||
| WD_15_1c | tpr57 (Luzon tectonic highland) | 0 | 1 | 1 | 2 | 0 | 4 | 1 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | vitric, microlitic, microphaneritic, argillitic, chert | ||
| WD_15_1b | tpr57 (Luzon tectonic highland) | 0 | 0 | 2 | 2 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 5 | 2 | 0 | vitric, microlitic, microphaneritic, argillitic, chert | ||
| WD_15_1a | tpr57 (Luzon tectonic highland) | 0 | 0 | 3 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 3 | 0 | vitric, microlitic, microphaneritic, argillitic, chert | ||
| WD_15_2a | tpr57 (Luzon tectonic highland) | 0 | 1 | 2 | 3 | 0 | 4 | 1 | 0 | 0 | 0 | 0 | 4 | 2 | 0 | vitric, microlitic, microphaneritic, argillitic, chert | ||
| WD_15_2b | tpr57 (Luzon tectonic highland) | 0 | 1 | 2 | 1 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 3 | 0 | vitric, microlitic, microphaneritic, argillitic, chert |
Feldspathic.
Feldspathic.
Feldspathic.
Lithic.
Lithic.
Lithic.
Feldspathic.
Feldspathic.
Feldspathic.
Feldspathic.
Feldspathic.
Lithic.
Lithic.
Lithic.
Lithic.
Heterogeneous sands of the tectonic highland temper class with red-brown vitric lithic fragments of mafic volcanic glass, iron oxides opaques, clinopyroxene and olivine mineral grains,chert and argillite lithic fragments with recrystallized ghosts of ovoid radiolarian tests visible in selected instances, microlitic lithic fragments derived from the groundmass of volcanic rocks.
Heterogeneous sands of the tectonic highland temper class with red-brown vitric lithic fragments of mafic volcanic glass, iron oxides opaques, clinopyroxene and olivine mineral grains,chert and argillite lithic fragments with recrystallized ghosts of ovoid radiolarian tests visible in selected instances, microlitic lithic fragments derived from the groundmass of volcanic rocks.
Heterogeneous sands of the tectonic highland temper class with red-brown vitric lithic fragments of mafic volcanic glass, iron oxides opaques, clinopyroxene and olivine mineral grains,chert and argillite lithic fragments with recrystallized ghosts of ovoid radiolarian tests visible in selected instances, microlitic lithic fragments derived from the groundmass of volcanic rocks.
Heterogeneous sands of the tectonic highland temper class with red-brown vitric lithic fragments of mafic volcanic glass, iron oxides opaques, clinopyroxene and olivine mineral grains,chert and argillite lithic fragments with recrystallized ghosts of ovoid radiolarian tests visible in selected instances, microlitic lithic fragments derived from the groundmass of volcanic rocks.
Heterogeneous sands of the tectonic highland temper class with red-brown vitric lithic fragments of mafic volcanic glass, iron oxides opaques, clinopyroxene and olivine mineral grains,chert and argillite lithic fragments with recrystallized ghosts of ovoid radiolarian tests visible in selected instances, microlitic lithic fragments derived from the groundmass of volcanic rocks.