Majolica (oxidized) light orange fabric; dark brown (PPL), dark brown (XP).
Homogenous matrix, non-calcareous with no optical activity.
- ca. 70-80%
Inclusions
Quartz (++; mono+, poly-), sedimentary rock detritus (-; quartz arenite), chert (+-), metamorphic rock detritus (-; low grade), muscovite mica (+-; el), O/Fe (+-; red and black iron oxides), CP/SP (+-; iron-rich).
The coarse fraction consists of medium sand, the fine fraction consists of fine sand, bimodal distribution. Grains are generally rounded to subrounded. Overall the fabric is very poorly sorted and moderately orientated, single to open spaced.
- ca. 15-25%
Voids
Large drying cracks along large parts of thin section, few planar/channel and vughs, no infill, well aligned.
- ca. 5%
Diagnostic features
The fabric is characterized by a homogenous oxidized matrix with no optical activity and low porosity. Dominant quartz inclusions with common chert, muscovite mica, opaques/iron oxides and iron-rich clay pellets, few sedimentary and metamorphic rock detritus. Overall very poorly sorted fabric.
Additional information
Similar to B0007a, but better firing conditions and finer fabric.
De Witte H. 1978. Arsenaalstraat: 18de-eeuwse faïenceindustrie. Het Brugs Ommeland 18, 4: 307.
Van Den Abeele 1986
Full reference
Van Den Abeele A. 1986. De faiencefabriek aan het Minnewater te Brugge (1750-1818). Handelingen van het Genootschap voor geschiedenis 123, 1-2: 61-105.
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