| Authors | Maryam Zohouriyan,Hossien Kohestani andarzi,Maryam Mortazavi Mehrizi, |
| Journal | Iranica Antiqua |
| Page number | 169-199 |
| Serial number | 60 |
| Volume number | 60 |
| Paper Type | Full Paper |
| Published At | 2026 |
| Journal Type | Typographic |
| Journal Country | Iran, Islamic Republic Of |
| Journal Index | JCR،Scopus |
| Keywords | Petrography, XRD, Provenance, Mineralogy, Gebri Mud B |
|---|
Abstract
As far as archaeological research is concerned, South Khorasan prov
ince is among the most influential regions in the era of the Parthians, who began
ruling Iran from 250 BCE. One of the most prominent archaeological sites in that
cultural region is Gebri Mud, located in the town of Mud, 30 km southeast of
Birjand, South Khorasan province. Although the typological study of its pottery
has been carried out in previous research, no laboratory analysis has been con
ducted on the provenance and mineralogical composition of this Parthian pottery,
despite the presence of Burnished Ware and Londo pottery.
The study therefore aims to address the following questions: To which region
does this pottery belong? And what is the structure of this pottery? The 14 pottery
samples from Tepeh Gebri Mud B were selected according to their color, shape
and decoration. Based on petrographic and XRD analyses, the authors selected
and compared the mineralogical composition of the pottery samples from Tepeh
Gebri Mud B with soils from five regions with a high probability to be pottery
production sites. The results indicate that the texture of the pottery samples can
be divided into three groups: fine-grained sand (125-250µm), medium-grained
sand (250-500µm), and coarse-grained sand (500-1000µm). The pottery compo
nents are divided into two categories: grain and matrix. The grains consist pre
dominantly of quartz (both monocrystalline and polycrystalline), which is the
most abundant mineral in the samples, as well as feldspar (orthoclase and plagio
clase), sandstone fragments (sedimentary and volcanic), micas (muscovite and
biotite), and heavy minerals (opaque).
Comparison of the mineralogical composition of the pottery with that of the stud
ied soils, together with the correlation with the regional geological map, indicates
that the provenance of the pottery is consistent with the Gebri region. The pottery
can therefore be considered local and imitative ware. Furthermore, the presence
of anorthite and sanidine phases in some samples, along with the absence of clay
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burnout, suggests that the pottery was produced at a high but controlled firing
temperature, indicating a high level of technological quality.
Keywords:
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