Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/11277
Authors: Burragato, Francesco* 
Di Nezza, Maria* 
Ferrazzoli, Adele Federica* 
Ricci, Marco* 
Editors: Bonifay, Michel 
Traglia, Jean-Christophe 
Title: Late Roman 1 amphora types produced at Elaiussa Sebaste.
Publisher: Archaeopress, British archaeological reports: International series, BAR International Series 1662 (II)
Issue Date: 2007
ISBN: 978 1 4073 0101 3
Keywords: Turkey
Elauissa Sebaste
Asia Minor
Byzantine
LR Amphora 1
mineralogical-petrographic groping
chemical grouping
Abstract: The Elaiussa Sebaste research project (Ayash, Turkey), carried out by University of Rome "La Sapienza" Archaeological Mission, and directed by Professor Eugenia Equini Schneider, started in 1995 and continues today. The ancient city of Elaiussa located on the south-eastern coast of Asia Minor as a Late Roman 1 amphorae and coarse wares production centre. The aim of this study was to get a basis for the mineralogical-petrographic and chemical grouping of Late Roman 1 amphorae and coarse wares found in Elaiussa. On the basis of archaeological classification, which describes different classes of use and their possible provenance with the following mineralogical and petrographic studies it is possible to partly confirm archaelogical data. The study of thin sections of ceramic samples shows hiatal and serial distribution of grain sizes and it is a good means to get geological information on the possible regions of manufacture. It is evident that the large fragments in a hiatal distribution pattern were not present in the clay from the beginning, but were added to it during the processing phase. Chemical compositions of ceramics is obtained by XRF analysis, using all major chemical elements and some minor elements (Zr, Zn, Ni, Ba, Cr), it is possible to generate groups of different provenance which often do not agree with geological setting of the area. The high Mg, Cr and Ni contents give us an indication on the geochimical origin of the clays. These elements are characteristics of ultrabasic rock usually connecred with ophiolites in agreement with the rock inclusions find from the study of thin sections.
Appears in Collections:Book chapters

Files in This Item:
File Description SizeFormat Existing users please Login
24_Burragatoetal_Lateromaine_2007.pdf4.85 MBAdobe PDF
Show full item record

Page view(s)

193
checked on Apr 24, 2024

Download(s)

39
checked on Apr 24, 2024

Google ScholarTM

Check

Altmetric