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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
 • Url: http://www.potsherd.org.uk/papers/cgmw/db/ts/211 • Author: • Last updated: 29 July, 2004 •