| 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 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 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 | Cal. | Quartz | Feldspar | Pyroxene | Amphibole | Opaques | Olivine | Biotite | Muscovite | Epidote | Garnet/ Spinel | Ig./Met. Rocks | Sed. Rocks | Grog | Lithics |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 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 |
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.