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The sherds
examined are mostly characterized by cobalt-blue designs which are
occasionally coupled with black, green and purple paintings. After grouping
the sherds according to their stylistic and color differences; petrographic,
X-ray diffraction, scanning electron microscope coupled with energy
dispersive X-ray and Fourier Transform Infrared analyses were carried out
for investigating the mineralogical and chemical properties. Most of the
ceramic samples have slip and glaze on both sides. The glaze part is mostly
fresh without any devitrification products. Bodies of the ceramics have
tones of reddish yellow and/or red, indicating abundant amount of iron in
their raw material. Grains consist mainly of metamorphic rock fragments
(quartz-mica schist), quartz, feldspar, hornblende, hematite and biotite.
Pyroxene, epidote, chert, muscovite, opaque minerals, chlorite are also
encountered. Micritic calcite occurs in some of the pores. Ceramic bodies
investigated are usually fine-grained and well-sorted. Clay raw material
used for the production of the ceramics seems to be originated from a
metamorphic source. Bodies usually show a low degree of vitrification with
few exceptions, indicating a rather simple technology with non-uniform and
low degree of firing, probably not exceeding 900°C. Technological
characteristics of the sherds examined do not seem to have changed much
between 14th and 16th century.
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