WASTE GLASS, VESSELS AND WINDOW‐PANES FROM THAMUSIDA (MOROCCO): GROUPING NATRON‐BASED BLUE–GREEN AND COLOURLESS ROMAN GLASSES
Identifieur interne : 000451 ( Istex/Corpus ); précédent : 000450; suivant : 000452WASTE GLASS, VESSELS AND WINDOW‐PANES FROM THAMUSIDA (MOROCCO): GROUPING NATRON‐BASED BLUE–GREEN AND COLOURLESS ROMAN GLASSES
Auteurs : E. Gliozzo ; A. Santagostino Barbone ; F. D'AcapitoSource :
- Archaeometry [ 0003-813X ] ; 2013-08.
English descriptors
Abstract
A collection of window‐panes, vessels and alleged waste from Thamusida has been investigated by OM, SEM–EDS, ICP–MS, ICP–OES and XAS at the Fe–K and Mn–K edges. Glass samples have been characterized as natron‐based soda–lime–silica glasses, with low magnesium and low potassium. The results have been compared with 43 reference groups available for ‘naturally coloured’ and colourless glasses of both Roman and later ages. Two main types were distinguished: RBGY 1 (Roman Blue–Green and Yellow 1) and RBGY 2 (Roman Blue–Green and Yellow 2). Given their compositional similarity to the Levantine I or, to a lesser extent, HIMT glasses, the Syrian–Palestinian coast for RBGY 2 and Egypt for the RBGY 1 have been suggested for their provenance. Most Thamusida samples have been assigned to the RBGY 2 type. A small group of Thamusida colourless vessels was included into the RC (Roman‐Colourless) compositional field; the latter still being defined. The alleged waste pieces may define a local production that should have been of secondary type. The investigations performed on local raw materials seem to discount the possibility of a primary glass‐making site. XAS measurements determined that Fe2+ contents ranging between 30 and 52% are able to assure an aqua blue colour; below 30%, the glasses turn light green or light yellow.
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DOI: 10.1111/j.1475-4754.2012.00696.x
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ISTEX:3B2B7429AA4EC2C11515C044E19DF3CDF2869626Le document en format XML
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Glass samples have been characterized as natron‐based soda–lime–silica glasses, with low magnesium and low potassium. The results have been compared with 43 reference groups available for ‘naturally coloured’ and colourless glasses of both Roman and later ages. Two main types were distinguished: RBGY 1 (Roman Blue–Green and Yellow 1) and RBGY 2 (Roman Blue–Green and Yellow 2). Given their compositional similarity to the Levantine I or, to a lesser extent, HIMT glasses, the Syrian–Palestinian coast for RBGY 2 and Egypt for the RBGY 1 have been suggested for their provenance. Most Thamusida samples have been assigned to the RBGY 2 type. A small group of Thamusida colourless vessels was included into the RC (Roman‐Colourless) compositional field; the latter still being defined. The alleged waste pieces may define a local production that should have been of secondary type. The investigations performed on local raw materials seem to discount the possibility of a primary glass‐making site. XAS measurements determined that Fe2+ contents ranging between 30 and 52% are able to assure an aqua blue colour; below 30%, the glasses turn light green or light yellow.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>E. GLIOZZO</name><affiliations><json:string>Department of Earth Sciences, University of Siena, via Laterina 8, 53100 Siena, Italy</json:string></affiliations></json:item><json:item><name>A. SANTAGOSTINO BARBONE</name><affiliations><json:string>Opificio delle pietre dure, Firenze, Italy</json:string></affiliations></json:item><json:item><name>F. 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Gliozzo, A. Santagostino Barbone and F. d'Acapito</title><title type="short">Waste glass, vessels and window‐panes from <i>Thamusida</i> (Morocco)</title></titleGroup><creators><creator creatorRole="author" xml:id="cr1" affiliationRef="#a1" corresponding="yes"><personName><givenNames>E.</givenNames><familyName>GLIOZZO</familyName></personName></creator><creator creatorRole="author" xml:id="cr2" affiliationRef="#a2"><personName><givenNames>A. SANTAGOSTINO</givenNames><familyName>BARBONE</familyName></personName></creator><creator creatorRole="author" xml:id="cr3" affiliationRef="#a3"><personName><givenNames>F.</givenNames><familyName>D'ACAPITO</familyName></personName></creator></creators><affiliationGroup><affiliation xml:id="a1" countryCode="IT"><unparsedAffiliation>Department of Earth Sciences, University of Siena, via Laterina 8, 53100 Siena, Italy</unparsedAffiliation></affiliation><affiliation xml:id="a2" countryCode="IT"><unparsedAffiliation>Opificio delle pietre dure, Firenze, Italy</unparsedAffiliation></affiliation><affiliation xml:id="a3" countryCode="FR"><unparsedAffiliation>CNR–IOM–OGG c/o ESRF, GILDA CRG, c/o ESRF BP220, F‐38043 Grenoble, France</unparsedAffiliation></affiliation></affiliationGroup><keywordGroup xml:lang="en"><keyword xml:id="k1">ROMAN GLASS</keyword><keyword xml:id="k2">XAS Fe–K Mn–K EDGE</keyword><keyword xml:id="k3"><i>THAMUSIDA</i></keyword><keyword xml:id="k4">MOROCCO</keyword><keyword xml:id="k5">PROVENANCE AND TECHNOLOGY</keyword></keywordGroup><fundingInfo><fundingAgency>CNR</fundingAgency></fundingInfo><fundingInfo><fundingAgency>INFN</fundingAgency></fundingInfo><fundingInfo><fundingAgency>ESRF</fundingAgency></fundingInfo><abstractGroup><abstract type="main" xml:lang="en"><p>A collection of window‐panes, vessels and alleged waste from <i>Thamusida</i> has been investigated by OM, SEM–EDS, ICP–MS, ICP–OES and XAS at the Fe–K and Mn–K edges. Glass samples have been characterized as natron‐based soda–lime–silica glasses, with low magnesium and low potassium. The results have been compared with 43 reference groups available for ‘naturally coloured’ and colourless glasses of both Roman and later ages. Two main types were distinguished: RBGY 1 (<span cssStyle="text-decoration:underline">R</span>oman <span cssStyle="text-decoration:underline">B</span>lue–<span cssStyle="text-decoration:underline">G</span>reen and <span cssStyle="text-decoration:underline">Y</span>ellow 1) and RBGY 2 (<span cssStyle="text-decoration:underline">R</span>oman <span cssStyle="text-decoration:underline">B</span>lue–<span cssStyle="text-decoration:underline">G</span>reen and <span cssStyle="text-decoration:underline">Y</span>ellow 2). Given their compositional similarity to the Levantine I or, to a lesser extent, HIMT glasses, the Syrian–Palestinian coast for RBGY 2 and Egypt for the RBGY 1 have been suggested for their provenance. Most <i>Thamusida</i> samples have been assigned to the RBGY 2 type. A small group of <i>Thamusida</i> colourless vessels was included into the RC (<span cssStyle="text-decoration:underline">R</span>oman‐<span cssStyle="text-decoration:underline">C</span>olourless) compositional field; the latter still being defined. The alleged waste pieces may define a local production that should have been of secondary type. The investigations performed on local raw materials seem to discount the possibility of a primary glass‐making site. XAS measurements determined that Fe<sup>2<i>+</i></sup> contents ranging between 30 and 52% are able to assure an aqua blue colour; below 30%, the glasses turn light green or light yellow.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>WASTE GLASS, VESSELS AND WINDOW‐PANES FROM THAMUSIDA (MOROCCO): GROUPING NATRON‐BASED BLUE–GREEN AND COLOURLESS ROMAN GLASSES</title></titleInfo><titleInfo type="abbreviated" lang="en"><title>Waste glass, vessels and window‐panes from Thamusida (Morocco)</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>WASTE GLASS, VESSELS AND WINDOW‐PANES FROM THAMUSIDA (MOROCCO): GROUPING NATRON‐BASED BLUE–GREEN AND COLOURLESS ROMAN GLASSES</title></titleInfo><name type="personal"><namePart type="given">E.</namePart><namePart type="family">GLIOZZO</namePart><affiliation>Department of Earth Sciences, University of Siena, via Laterina 8, 53100 Siena, Italy</affiliation><affiliation>E-mail: gliozzo@unisi.it</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">A. SANTAGOSTINO</namePart><namePart type="family">BARBONE</namePart><affiliation>Opificio delle pietre dure, Firenze, Italy</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">F.</namePart><namePart type="family">D'ACAPITO</namePart><affiliation>CNR–IOM–OGG c/o ESRF, GILDA CRG, c/o ESRF BP220, F‐38043 Grenoble, France</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article"></genre><originInfo><publisher>Blackwell Publishing Ltd</publisher><place><placeTerm type="text">Oxford, UK</placeTerm></place><dateIssued encoding="w3cdtf">2013-08</dateIssued><edition>Received 13 March 2012; accepted 11 April 2012</edition><copyrightDate encoding="w3cdtf">2013</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType><extent unit="figures">7</extent><extent unit="tables">7</extent><extent unit="references">63</extent><extent unit="words">10201</extent></physicalDescription><abstract lang="en">A collection of window‐panes, vessels and alleged waste from Thamusida has been investigated by OM, SEM–EDS, ICP–MS, ICP–OES and XAS at the Fe–K and Mn–K edges. Glass samples have been characterized as natron‐based soda–lime–silica glasses, with low magnesium and low potassium. The results have been compared with 43 reference groups available for ‘naturally coloured’ and colourless glasses of both Roman and later ages. Two main types were distinguished: RBGY 1 (Roman Blue–Green and Yellow 1) and RBGY 2 (Roman Blue–Green and Yellow 2). Given their compositional similarity to the Levantine I or, to a lesser extent, HIMT glasses, the Syrian–Palestinian coast for RBGY 2 and Egypt for the RBGY 1 have been suggested for their provenance. Most Thamusida samples have been assigned to the RBGY 2 type. A small group of Thamusida colourless vessels was included into the RC (Roman‐Colourless) compositional field; the latter still being defined. The alleged waste pieces may define a local production that should have been of secondary type. The investigations performed on local raw materials seem to discount the possibility of a primary glass‐making site. XAS measurements determined that Fe2+ contents ranging between 30 and 52% are able to assure an aqua blue colour; below 30%, the glasses turn light green or light yellow.</abstract><note type="funding">CNR</note><note type="funding">INFN</note><note type="funding">ESRF</note><subject lang="en"><genre>keywords</genre><topic>ROMAN GLASS</topic><topic>XAS Fe–K Mn–K EDGE</topic><topic>THAMUSIDA</topic><topic>MOROCCO</topic><topic>PROVENANCE AND TECHNOLOGY</topic></subject><relatedItem type="host"><titleInfo><title>Archaeometry</title></titleInfo><genre type="journal">journal</genre><subject><genre>article-category</genre><topic>Original Article</topic></subject><identifier type="ISSN">0003-813X</identifier><identifier type="eISSN">1475-4754</identifier><identifier type="DOI">10.1111/(ISSN)1475-4754</identifier><identifier type="PublisherID">ARCM</identifier><part><date>2013</date><detail type="volume"><caption>vol.</caption><number>55</number></detail><detail type="issue"><caption>no.</caption><number>4</number></detail><extent unit="pages"><start>609</start><end>639</end><total>31</total></extent></part></relatedItem><identifier type="istex">3B2B7429AA4EC2C11515C044E19DF3CDF2869626</identifier><identifier type="DOI">10.1111/j.1475-4754.2012.00696.x</identifier><identifier type="ArticleID">ARCM696</identifier><accessCondition type="use and reproduction" contentType="copyright">© 2013 University of Oxford© 2012 University of Oxford</accessCondition><recordInfo><recordContentSource>WILEY</recordContentSource><recordOrigin>Blackwell Publishing Ltd</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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