A mineralogical study of Late Bronze Age ceramics from Palatca (Transylvania, Romania)

Our paper studies the mineralogical and petrographical characteristics of 28 ceramic fragments that were excavated in the village of Palatca, Transylvania (Romania). Optical microscopy, X-Ray powder diffraction (XRD), scanning electron microscopy (SEM), grain size analyses, and porosity measurements...

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Main Authors: Lucretia Ghergari, Carmen Stâncel
Format: Article
Language:English
Published: Cluj University Press 2012-01-01
Series:Studia Universitatis Babes-Bolyai: Geologia
Online Access:http://scholarcommons.usf.edu/geologia/vol57/iss1/art2/
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spelling doaj-1d4c396ad3b4437fb5a524f659fd2fbc2020-11-24T21:35:59ZengCluj University PressStudia Universitatis Babes-Bolyai: Geologia1221-08031937-86022012-01-015711321A mineralogical study of Late Bronze Age ceramics from Palatca (Transylvania, Romania)Lucretia Ghergari0Carmen Stâncel1Department of Geology, Babes-Bolyai University, Cluj-Napoca, RomaniaDepartment of Geology, Babes-Bolyai University, Cluj-Napoca, RomaniaOur paper studies the mineralogical and petrographical characteristics of 28 ceramic fragments that were excavated in the village of Palatca, Transylvania (Romania). Optical microscopy, X-Ray powder diffraction (XRD), scanning electron microscopy (SEM), grain size analyses, and porosity measurements were used to investigate the samples. Our objective was to describe or reconstruct the corresponding products and to elucidate the manufacturing process, the firing techniques, and the transformation pathways. Based on our results, we conclude that the Late Bronze Age ceramics (1600-1300 BC) were produced from clay and temper material such as river sand and ceramoclasts. It has been modeled by hand and fired between 800 and 950°C. For most samples, we can narrow the temperature range to 850-900°C. We interpret the data further from a geoarchaeological point of view with respect to the historical evolution of the local culture. http://scholarcommons.usf.edu/geologia/vol57/iss1/art2/
collection DOAJ
language English
format Article
sources DOAJ
author Lucretia Ghergari
Carmen Stâncel
spellingShingle Lucretia Ghergari
Carmen Stâncel
A mineralogical study of Late Bronze Age ceramics from Palatca (Transylvania, Romania)
Studia Universitatis Babes-Bolyai: Geologia
author_facet Lucretia Ghergari
Carmen Stâncel
author_sort Lucretia Ghergari
title A mineralogical study of Late Bronze Age ceramics from Palatca (Transylvania, Romania)
title_short A mineralogical study of Late Bronze Age ceramics from Palatca (Transylvania, Romania)
title_full A mineralogical study of Late Bronze Age ceramics from Palatca (Transylvania, Romania)
title_fullStr A mineralogical study of Late Bronze Age ceramics from Palatca (Transylvania, Romania)
title_full_unstemmed A mineralogical study of Late Bronze Age ceramics from Palatca (Transylvania, Romania)
title_sort mineralogical study of late bronze age ceramics from palatca (transylvania, romania)
publisher Cluj University Press
series Studia Universitatis Babes-Bolyai: Geologia
issn 1221-0803
1937-8602
publishDate 2012-01-01
description Our paper studies the mineralogical and petrographical characteristics of 28 ceramic fragments that were excavated in the village of Palatca, Transylvania (Romania). Optical microscopy, X-Ray powder diffraction (XRD), scanning electron microscopy (SEM), grain size analyses, and porosity measurements were used to investigate the samples. Our objective was to describe or reconstruct the corresponding products and to elucidate the manufacturing process, the firing techniques, and the transformation pathways. Based on our results, we conclude that the Late Bronze Age ceramics (1600-1300 BC) were produced from clay and temper material such as river sand and ceramoclasts. It has been modeled by hand and fired between 800 and 950°C. For most samples, we can narrow the temperature range to 850-900°C. We interpret the data further from a geoarchaeological point of view with respect to the historical evolution of the local culture.
url http://scholarcommons.usf.edu/geologia/vol57/iss1/art2/
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