Miocene magnesian andesites and dacites, Evia, Greece: adakites associated with subducting slab detachment and extension
Identifieur interne : 000334 ( Istex/Corpus ); précédent : 000333; suivant : 000335Miocene magnesian andesites and dacites, Evia, Greece: adakites associated with subducting slab detachment and extension
Auteurs : Georgia Pe-Piper ; David J. W. PiperSource :
- Lithos [ 0024-4937 ] ; 1994.
English descriptors
- KwdEn :
- Adakites, Amphibole, Andesite, Aphyric, Aphyric dacite, Biotite, Boninite, Boninites, Bronzite, Bronzite phenocrysts, Clast, Clinopyroxene, Contrib, Crust, Crystallisation, Dacite, Defant, Early miocene, Earth planet, Evia, Felsic, Felsic pyroclastic rocks, Fractional crystallisation, Geol, Groundmass, High temperatures, Hornblende, Igneous rocks, Isotope, Isotopic composition, Lacustrine, Lava, Lett, Limited extent, Magma, Magnesian, Magnesian andesites, Middle miocene, Mineral chemistry, Miocene, Northern greece, Oceanic, Opaque rims, Orion, Orthopyroxene, Oxylithos, Oxylithos andesite, Oxylithos andesites, Oxylithos rocks, Oxylithos volcanics, Petrol, Phenocrysts, Phlogopite, Piper, Plagioclase, Plagioclase phenocrysts, Porphyritic, Porphyritic dacite, Pyroclastic, Pyroxene, Quartz, Rhyolite, Sio2, Subducted, Subducted slab, Subduction, Tatsumi, Trace elements, Unwin hyman, Volcanic rocks, Volcanism, Western aegean, Xenolith.
- Teeft :
- Adakites, Amphibole, Andesite, Aphyric, Aphyric dacite, Biotite, Boninite, Boninites, Bronzite, Bronzite phenocrysts, Clast, Clinopyroxene, Contrib, Crust, Crystallisation, Dacite, Defant, Early miocene, Earth planet, Evia, Felsic, Felsic pyroclastic rocks, Fractional crystallisation, Geol, Groundmass, High temperatures, Hornblende, Igneous rocks, Isotope, Isotopic composition, Lacustrine, Lava, Lett, Limited extent, Magma, Magnesian, Magnesian andesites, Middle miocene, Mineral chemistry, Miocene, Northern greece, Oceanic, Opaque rims, Orion, Orthopyroxene, Oxylithos, Oxylithos andesite, Oxylithos andesites, Oxylithos rocks, Oxylithos volcanics, Petrol, Phenocrysts, Phlogopite, Piper, Plagioclase, Plagioclase phenocrysts, Porphyritic, Porphyritic dacite, Pyroclastic, Pyroxene, Quartz, Rhyolite, Sio2, Subducted, Subducted slab, Subduction, Tatsumi, Trace elements, Unwin hyman, Volcanic rocks, Volcanism, Western aegean, Xenolith.
Abstract
Abstract: Mid-Miocene volcanic rocks are rare in the Aegean region, although early Miocene and late Miocene-Quaternary volcanism is widespread. At Oxylithos (island of Evia), 14 Ma dacites form a dome or sub-volcanic complex. Phreatomagmatic eruptions formed nearby rhyolitic pyroclastic surge deposits. The calc-alkaline dacites contain bronzite, Mg-rich clinopyroxene, phlogopite and plagioclase phenocrysts. The magma results from mixing of a Mg-rich andesitic magma, similar to that in the nearby island of Skyros, with more felsic magmas represented by the rhyolitic pyroclastics. The dacites are geochemically similar to adakites, which are derived by partial melting of eclogitic subducted oceanic crust and have low Y and Yb and high SrY ratio. 87Sr86Sr≈0.7095 is found in both dacite and rhyolite. Lead isotopic composition from the high-Mg andesite from Skyros, with 207Pb204Pb= 15.70 and 208Pb204Pb= 38.90, forms a linear trend with Evia dacite and rhyolite with 207Pb204Pb= 15.71 and 208Pb204Pb= 39.05. The high temperatures required to produce such magma resulted from decompression due to extension of the Aegean basin at the same time as the initial intrusion of the detached subducted slab in the western Aegean that has been imaged by seismic tomography. The Oxylithos rocks extend the known occurrences of adakite series rocks: this series is not restricted to sites with subduction of young oceanic crust.
Url:
DOI: 10.1016/0024-4937(94)90004-3
Links to Exploration step
ISTEX:A0FE82A1D8D44140075738A292C0057A63F20130Le document en format XML
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At Oxylithos (island of Evia), 14 Ma dacites form a dome or sub-volcanic complex. Phreatomagmatic eruptions formed nearby rhyolitic pyroclastic surge deposits. The calc-alkaline dacites contain bronzite, Mg-rich clinopyroxene, phlogopite and plagioclase phenocrysts. The magma results from mixing of a Mg-rich andesitic magma, similar to that in the nearby island of Skyros, with more felsic magmas represented by the rhyolitic pyroclastics. The dacites are geochemically similar to adakites, which are derived by partial melting of eclogitic subducted oceanic crust and have low Y and Yb and high SrY ratio. 87Sr86Sr≈0.7095 is found in both dacite and rhyolite. Lead isotopic composition from the high-Mg andesite from Skyros, with 207Pb204Pb= 15.70 and 208Pb204Pb= 38.90, forms a linear trend with Evia dacite and rhyolite with 207Pb204Pb= 15.71 and 208Pb204Pb= 39.05. The high temperatures required to produce such magma resulted from decompression due to extension of the Aegean basin at the same time as the initial intrusion of the detached subducted slab in the western Aegean that has been imaged by seismic tomography. The Oxylithos rocks extend the known occurrences of adakite series rocks: this series is not restricted to sites with subduction of young oceanic crust.</div></front></TEI><istex><corpusName>elsevier</corpusName><keywords><teeft><json:string>dacite</json:string><json:string>andesite</json:string><json:string>oxylithos</json:string><json:string>rhyolite</json:string><json:string>miocene</json:string><json:string>magma</json:string><json:string>orion</json:string><json:string>phenocrysts</json:string><json:string>amphibole</json:string><json:string>porphyritic</json:string><json:string>plagioclase</json:string><json:string>evia</json:string><json:string>piper</json:string><json:string>pyroclastic</json:string><json:string>clast</json:string><json:string>pyroxene</json:string><json:string>adakites</json:string><json:string>groundmass</json:string><json:string>sio2</json:string><json:string>subduction</json:string><json:string>felsic</json:string><json:string>volcanism</json:string><json:string>subducted</json:string><json:string>orthopyroxene</json:string><json:string>petrol</json:string><json:string>tatsumi</json:string><json:string>oceanic</json:string><json:string>hornblende</json:string><json:string>geol</json:string><json:string>bronzite</json:string><json:string>crystallisation</json:string><json:string>aphyric</json:string><json:string>isotope</json:string><json:string>boninites</json:string><json:string>magnesian</json:string><json:string>biotite</json:string><json:string>contrib</json:string><json:string>porphyritic dacite</json:string><json:string>lacustrine</json:string><json:string>defant</json:string><json:string>clinopyroxene</json:string><json:string>phlogopite</json:string><json:string>boninite</json:string><json:string>lett</json:string><json:string>xenolith</json:string><json:string>crust</json:string><json:string>earth planet</json:string><json:string>early miocene</json:string><json:string>quartz</json:string><json:string>oxylithos rocks</json:string><json:string>plagioclase phenocrysts</json:string><json:string>magnesian andesites</json:string><json:string>isotopic composition</json:string><json:string>lava</json:string><json:string>western aegean</json:string><json:string>oxylithos andesites</json:string><json:string>fractional crystallisation</json:string><json:string>high temperatures</json:string><json:string>volcanic rocks</json:string><json:string>subducted slab</json:string><json:string>northern greece</json:string><json:string>unwin hyman</json:string><json:string>opaque rims</json:string><json:string>mineral chemistry</json:string><json:string>bronzite phenocrysts</json:string><json:string>oxylithos andesite</json:string><json:string>igneous rocks</json:string><json:string>trace elements</json:string><json:string>felsic pyroclastic rocks</json:string><json:string>oxylithos volcanics</json:string><json:string>middle miocene</json:string><json:string>limited extent</json:string><json:string>aphyric dacite</json:string></teeft></keywords><author><json:item><name>Georgia Pe-Piper</name><affiliations><json:string>Department of Geology, Saint Mary's University, Halifax, N.S. B3H 3C3, Canada</json:string></affiliations></json:item><json:item><name>David J.W. Piper</name><affiliations><json:string>Atlantic Geoscience Centre, Geological Survey of Canada, Bedford Institute of Oceanography, P.O. Box 1006, Dartmouth, N.S. B2Y 4A2, Canada</json:string></affiliations></json:item></author><language><json:string>eng</json:string></language><originalGenre><json:string>Full-length article</json:string></originalGenre><abstract>Mid-Miocene volcanic rocks are rare in the Aegean region, although early Miocene and late Miocene-Quaternary volcanism is widespread. At Oxylithos (island of Evia), 14 Ma dacites form a dome or sub-volcanic complex. Phreatomagmatic eruptions formed nearby rhyolitic pyroclastic surge deposits. The calc-alkaline dacites contain bronzite, Mg-rich clinopyroxene, phlogopite and plagioclase phenocrysts. The magma results from mixing of a Mg-rich andesitic magma, similar to that in the nearby island of Skyros, with more felsic magmas represented by the rhyolitic pyroclastics. The dacites are geochemically similar to adakites, which are derived by partial melting of eclogitic subducted oceanic crust and have low Y and Yb and high SrY ratio. 87Sr86Sr≈0.7095 is found in both dacite and rhyolite. Lead isotopic composition from the high-Mg andesite from Skyros, with 207Pb204Pb= 15.70 and 208Pb204Pb= 38.90, forms a linear trend with Evia dacite and rhyolite with 207Pb204Pb= 15.71 and 208Pb204Pb= 39.05. The high temperatures required to produce such magma resulted from decompression due to extension of the Aegean basin at the same time as the initial intrusion of the detached subducted slab in the western Aegean that has been imaged by seismic tomography. The Oxylithos rocks extend the known occurrences of adakite series rocks: this series is not restricted to sites with subduction of young oceanic crust.</abstract><qualityIndicators><score>8.032</score><pdfVersion>1.4</pdfVersion><pdfPageSize>540 x 749 pts</pdfPageSize><refBibsNative>true</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>1414</abstractCharCount><pdfWordCount>6479</pdfWordCount><pdfCharCount>44727</pdfCharCount><pdfPageCount>16</pdfPageCount><abstractWordCount>211</abstractWordCount></qualityIndicators><title>Miocene magnesian andesites and dacites, Evia, Greece: adakites associated with subducting slab detachment and extension</title><pii><json:string>0024-4937(94)90004-3</json:string></pii><genre><json:string>research-article</json:string></genre><serie><title>Thèse 3ème cycle</title><language><json:string>unknown</json:string></language><pages><first>173</first></pages></serie><host><title>Lithos</title><language><json:string>unknown</json:string></language><publicationDate>1994</publicationDate><issn><json:string>0024-4937</json:string></issn><pii><json:string>S0024-4937(00)X0160-0</json:string></pii><volume>31</volume><issue>3–4</issue><pages><first>125</first><last>140</last></pages><genre><json:string>journal</json:string></genre></host><categories><wos><json:string>science</json:string><json:string>mineralogy</json:string><json:string>geochemistry & geophysics</json:string></wos><scienceMetrix><json:string>natural sciences</json:string><json:string>earth & environmental sciences</json:string><json:string>geochemistry & geophysics</json:string></scienceMetrix><inist><json:string>sciences appliquees, technologies et medecines</json:string><json:string>sciences exactes et technologie</json:string><json:string>terre, ocean, espace</json:string><json:string>sciences de la terre</json:string></inist></categories><publicationDate>1994</publicationDate><copyrightDate>1994</copyrightDate><doi><json:string>10.1016/0024-4937(94)90004-3</json:string></doi><id>A0FE82A1D8D44140075738A292C0057A63F20130</id><score>1</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/A0FE82A1D8D44140075738A292C0057A63F20130/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/A0FE82A1D8D44140075738A292C0057A63F20130/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/A0FE82A1D8D44140075738A292C0057A63F20130/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a">Miocene magnesian andesites and dacites, Evia, Greece: adakites associated with subducting slab detachment and extension</title></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>ELSEVIER</publisher><availability><p>ELSEVIER</p></availability><date>1994</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a">Miocene magnesian andesites and dacites, Evia, Greece: adakites associated with subducting slab detachment and extension</title><author xml:id="author-0000"><persName><forename type="first">Georgia</forename><surname>Pe-Piper</surname></persName><affiliation>Department of Geology, Saint Mary's University, Halifax, N.S. B3H 3C3, Canada</affiliation></author><author xml:id="author-0001"><persName><forename type="first">David J.W.</forename><surname>Piper</surname></persName><affiliation>Atlantic Geoscience Centre, Geological Survey of Canada, Bedford Institute of Oceanography, P.O. Box 1006, Dartmouth, N.S. B2Y 4A2, Canada</affiliation></author><idno type="istex">A0FE82A1D8D44140075738A292C0057A63F20130</idno><idno type="DOI">10.1016/0024-4937(94)90004-3</idno><idno type="PII">0024-4937(94)90004-3</idno></analytic><monogr><title level="j">Lithos</title><title level="j" type="abbrev">LITHOS</title><idno type="pISSN">0024-4937</idno><idno type="PII">S0024-4937(00)X0160-0</idno><imprint><publisher>ELSEVIER</publisher><date type="published" when="1994"></date><biblScope unit="volume">31</biblScope><biblScope unit="issue">3–4</biblScope><biblScope unit="page" from="125">125</biblScope><biblScope unit="page" to="140">140</biblScope></imprint></monogr></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1994</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Mid-Miocene volcanic rocks are rare in the Aegean region, although early Miocene and late Miocene-Quaternary volcanism is widespread. At Oxylithos (island of Evia), 14 Ma dacites form a dome or sub-volcanic complex. Phreatomagmatic eruptions formed nearby rhyolitic pyroclastic surge deposits. The calc-alkaline dacites contain bronzite, Mg-rich clinopyroxene, phlogopite and plagioclase phenocrysts. The magma results from mixing of a Mg-rich andesitic magma, similar to that in the nearby island of Skyros, with more felsic magmas represented by the rhyolitic pyroclastics. The dacites are geochemically similar to adakites, which are derived by partial melting of eclogitic subducted oceanic crust and have low Y and Yb and high SrY ratio. 87Sr86Sr≈0.7095 is found in both dacite and rhyolite. Lead isotopic composition from the high-Mg andesite from Skyros, with 207Pb204Pb= 15.70 and 208Pb204Pb= 38.90, forms a linear trend with Evia dacite and rhyolite with 207Pb204Pb= 15.71 and 208Pb204Pb= 39.05. The high temperatures required to produce such magma resulted from decompression due to extension of the Aegean basin at the same time as the initial intrusion of the detached subducted slab in the western Aegean that has been imaged by seismic tomography. The Oxylithos rocks extend the known occurrences of adakite series rocks: this series is not restricted to sites with subduction of young oceanic crust.</p></abstract></profileDesc><revisionDesc><change when="1994">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/A0FE82A1D8D44140075738A292C0057A63F20130/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Elsevier, elements deleted: tail"><istex:xmlDeclaration>version="1.0" encoding="utf-8"</istex:xmlDeclaration><istex:docType PUBLIC="-//ES//DTD journal article DTD version 4.5.2//EN//XML" URI="art452.dtd" name="istex:docType"></istex:docType><istex:document><converted-article version="4.5.2" docsubtype="fla"><item-info><jid>LITHOS</jid><aid>94900043</aid><ce:pii>0024-4937(94)90004-3</ce:pii><ce:doi>10.1016/0024-4937(94)90004-3</ce:doi><ce:copyright type="unknown" year="1994"></ce:copyright></item-info><head><ce:title>Miocene magnesian andesites and dacites, Evia, Greece: adakites associated with subducting slab detachment and extension</ce:title><ce:author-group><ce:author><ce:given-name>Georgia</ce:given-name><ce:surname>Pe-Piper</ce:surname><ce:cross-ref refid="AFF1"><ce:sup>a</ce:sup></ce:cross-ref></ce:author><ce:author><ce:given-name>David J.W.</ce:given-name><ce:surname>Piper</ce:surname><ce:cross-ref refid="AFF2"><ce:sup>b</ce:sup></ce:cross-ref></ce:author><ce:affiliation id="AFF1"><ce:label>a</ce:label><ce:textfn>Department of Geology, Saint Mary's University, Halifax, N.S. B3H 3C3, Canada</ce:textfn></ce:affiliation><ce:affiliation id="AFF2"><ce:label>b</ce:label><ce:textfn>Atlantic Geoscience Centre, Geological Survey of Canada, Bedford Institute of Oceanography, P.O. Box 1006, Dartmouth, N.S. B2Y 4A2, Canada</ce:textfn></ce:affiliation></ce:author-group><ce:date-received day="3" month="12" year="1992"></ce:date-received><ce:date-accepted day="18" month="5" year="1993"></ce:date-accepted><ce:abstract><ce:section-title>Abstract</ce:section-title><ce:abstract-sec><ce:simple-para>Mid-Miocene volcanic rocks are rare in the Aegean region, although early Miocene and late Miocene-Quaternary volcanism is widespread. At Oxylithos (island of Evia), 14 Ma dacites form a dome or sub-volcanic complex. Phreatomagmatic eruptions formed nearby rhyolitic pyroclastic surge deposits. The calc-alkaline dacites contain bronzite, Mg-rich clinopyroxene, phlogopite and plagioclase phenocrysts. The magma results from mixing of a Mg-rich andesitic magma, similar to that in the nearby island of Skyros, with more felsic magmas represented by the rhyolitic pyroclastics. The dacites are geochemically similar to adakites, which are derived by partial melting of eclogitic subducted oceanic crust and have low Y and Yb and high <math altimg="si1.gif"><fr shape="sol"><nu><rm>Sr</rm></nu><de><rm>Y</rm></de></fr></math> ratio. <math altimg="si2.gif"><fr shape="sol"><nu><sup>87</sup><rm>Sr</rm></nu><de><sup>86</sup><rm>Sr</rm></de></fr>≈0.7095</math> is found in both dacite and rhyolite. Lead isotopic composition from the high-Mg andesite from Skyros, with <math altimg="si3.gif"><fr shape="sol"><nu><sup>207</sup><rm>Pb</rm></nu><de><sup>204</sup><rm>Pb</rm></de></fr>= 15.70</math> and <math altimg="si4.gif"><fr shape="sol"><nu><sup>208</sup><rm>Pb</rm></nu><de><sup>204</sup><rm>Pb</rm></de></fr>= 38.90</math>, forms a linear trend with Evia dacite and rhyolite with <math altimg="si5.gif"><fr shape="sol"><nu><sup>207</sup><rm>Pb</rm></nu><de><sup>204</sup><rm>Pb</rm></de></fr>= 15.71</math> and <math altimg="si6.gif"><fr shape="sol"><nu><sup>208</sup><rm>Pb</rm></nu><de><sup>204</sup><rm>Pb</rm></de></fr>= 39.05</math>. The high temperatures required to produce such magma resulted from decompression due to extension of the Aegean basin at the same time as the initial intrusion of the detached subducted slab in the western Aegean that has been imaged by seismic tomography. The Oxylithos rocks extend the known occurrences of adakite series rocks: this series is not restricted to sites with subduction of young oceanic crust.</ce:simple-para></ce:abstract-sec></ce:abstract></head></converted-article></istex:document></istex:metadataXml><mods version="3.6"><titleInfo><title>Miocene magnesian andesites and dacites, Evia, Greece: adakites associated with subducting slab detachment and extension</title></titleInfo><titleInfo type="alternative" contentType="CDATA"><title>Miocene magnesian andesites and dacites, Evia, Greece: adakites associated with subducting slab detachment and extension</title></titleInfo><name type="personal"><namePart type="given">Georgia</namePart><namePart type="family">Pe-Piper</namePart><affiliation>Department of Geology, Saint Mary's University, Halifax, N.S. B3H 3C3, Canada</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">David J.W.</namePart><namePart type="family">Piper</namePart><affiliation>Atlantic Geoscience Centre, Geological Survey of Canada, Bedford Institute of Oceanography, P.O. Box 1006, Dartmouth, N.S. B2Y 4A2, Canada</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="Full-length article" authority="ISTEX" authorityURI="https://content-type.data.istex.fr" valueURI="https://content-type.data.istex.fr/ark:/67375/XTP-1JC4F85T-7">research-article</genre><originInfo><publisher>ELSEVIER</publisher><dateIssued encoding="w3cdtf">1994</dateIssued><copyrightDate encoding="w3cdtf">1994</copyrightDate></originInfo><language><languageTerm type="code" authority="iso639-2b">eng</languageTerm><languageTerm type="code" authority="rfc3066">en</languageTerm></language><abstract lang="en">Abstract: Mid-Miocene volcanic rocks are rare in the Aegean region, although early Miocene and late Miocene-Quaternary volcanism is widespread. At Oxylithos (island of Evia), 14 Ma dacites form a dome or sub-volcanic complex. Phreatomagmatic eruptions formed nearby rhyolitic pyroclastic surge deposits. The calc-alkaline dacites contain bronzite, Mg-rich clinopyroxene, phlogopite and plagioclase phenocrysts. The magma results from mixing of a Mg-rich andesitic magma, similar to that in the nearby island of Skyros, with more felsic magmas represented by the rhyolitic pyroclastics. The dacites are geochemically similar to adakites, which are derived by partial melting of eclogitic subducted oceanic crust and have low Y and Yb and high SrY ratio. 87Sr86Sr≈0.7095 is found in both dacite and rhyolite. Lead isotopic composition from the high-Mg andesite from Skyros, with 207Pb204Pb= 15.70 and 208Pb204Pb= 38.90, forms a linear trend with Evia dacite and rhyolite with 207Pb204Pb= 15.71 and 208Pb204Pb= 39.05. The high temperatures required to produce such magma resulted from decompression due to extension of the Aegean basin at the same time as the initial intrusion of the detached subducted slab in the western Aegean that has been imaged by seismic tomography. The Oxylithos rocks extend the known occurrences of adakite series rocks: this series is not restricted to sites with subduction of young oceanic crust.</abstract><relatedItem type="host"><titleInfo><title>Lithos</title></titleInfo><titleInfo type="abbreviated"><title>LITHOS</title></titleInfo><genre type="journal" authority="ISTEX" authorityURI="https://publication-type.data.istex.fr" valueURI="https://publication-type.data.istex.fr/ark:/67375/JMC-0GLKJH51-B">journal</genre><originInfo><publisher>ELSEVIER</publisher><dateIssued encoding="w3cdtf">199401</dateIssued></originInfo><identifier type="ISSN">0024-4937</identifier><identifier type="PII">S0024-4937(00)X0160-0</identifier><part><date>199401</date><detail type="volume"><number>31</number><caption>vol.</caption></detail><detail type="issue"><number>3–4</number><caption>no.</caption></detail><extent unit="issue-pages"><start>65</start><end>237</end></extent><extent unit="pages"><start>125</start><end>140</end></extent></part></relatedItem><identifier type="istex">A0FE82A1D8D44140075738A292C0057A63F20130</identifier><identifier type="ark">ark:/67375/6H6-GMN8TLV2-D</identifier><identifier type="DOI">10.1016/0024-4937(94)90004-3</identifier><identifier type="PII">0024-4937(94)90004-3</identifier><recordInfo><recordContentSource authority="ISTEX" authorityURI="https://loaded-corpus.data.istex.fr" valueURI="https://loaded-corpus.data.istex.fr/ark:/67375/XBH-HKKZVM7B-M">elsevier</recordContentSource></recordInfo></mods><json:item><extension>json</extension><original>false</original><mimetype>application/json</mimetype><uri>https://api.istex.fr/document/A0FE82A1D8D44140075738A292C0057A63F20130/metadata/json</uri></json:item></metadata></istex></record>Pour manipuler ce document sous Unix (Dilib)
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