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Camulodunum type 262, le type Besançon and Central Gaulish granite-tempered ware
| TS ID |
211 |
| Site name |
Chartres |
| ref |
C23.150.13.V23 |
| form |
Cam 262 |
| petrology |
TF2 ’Standard fabric‘ /cf.B134 |
| Thin section |
TS
IF: plagioclase, orthoclase biotite mica feldspar
- shattered? crushed?
weathered rock not moved from where it was weathered.
Inclusion looks like glass (?obsidian)
Pyroxene, lava - fresh feld phenocryst (2 egs)
Volcanic rather than lava as such
Basically granitic, feldspars much fresher,
typical of volcanic feldspar - Massif Central
basic igneous rock and opaque inclusions |
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