This petro fabric relates to Palaepaphos Hadjiabdoulla mudstone-tempered; the difference
between the two is that in this fabric the majority of the nonplastic components relates to an ophiolitic environment and the fragments of the
mudstone are not only fewer in number but also smaller in size and more rounded.This indicates that in this case the mudstone in not added as temper by the potter but occurs naturally in the alluvial raw material.
This petro fabric relates to Palaepaphos Hadjiabdoulla mudstone-tempered; the difference
between the two is that in this fabric the majority of the nonplastic components relates to an ophiolitic environment and the fragments of the
mudstone are not only fewer in number but also smaller in size and more rounded.This indicates that in this case the mudstone in not added as temper by the potter but occurs naturally in the alluvial raw material.
