Magma mixing at Nisyros volcano, as inferred from incompatible trace-element systematics
Identifieur interne : 000017 ( Istex/Corpus ); précédent : 000016; suivant : 000018Magma mixing at Nisyros volcano, as inferred from incompatible trace-element systematics
Auteurs : Karen St. Seymour ; Dimitri VlassopoulosSource :
- Journal of Volcanology and Geothermal Research [ 0377-0273 ] ; 1992.
English descriptors
- KwdEn :
- Amphibole, Andesite, Andesite inclusion, Andesitic, Andesitic inclusions, Apatite, Basalt, Basaltic, Basaltic andesite, Basaltic andesites, Caldera, Caldera collapse, Clinopyroxene, Companion plots, Compositional, Concordia university, Contrib, Crustal, Crustal assimilation, Crystal fractionation, Dacite, Dacitic, Felsic, Fractional crystallization, Fractionation, Hyperbolic distributions, Inclusion, Incompatible, Labr, Lalonde, Langmuir, Lava, Linear trend, Mafic, Mafic glass, Mafic liquids, Magma, Magmatic, Major elements, Mineral chemistry, Nisyros, Nisyros lavas, Nisyros volcano, Olivine, Opaque oxides, Orthopyroxene, Oxide, Paola, Parentheses population, Parentheses representative analyses, Pearce, Petrogenetic, Petrol, Phenocrysts, Plagioclase, Plagioclase phenocrysts, Postcaldera dacites, Pumice, Pumiceous, Pyroclastic, Rhyodacite, Rhyodacite flows, Rhyodacites, Rhyolite, Seymour, Silicic, Silicic andesites, Sio2, Source region, Subaerial, Subaerial andesites, Systematics, Tio2, Trace elements, Vlassopoulos, Vlassopoulos table, Volcanic, Volcanic rocks, Volcanism, Volcano, Volcanol, Wyers.
- Teeft :
- Amphibole, Andesite, Andesite inclusion, Andesitic, Andesitic inclusions, Apatite, Basalt, Basaltic, Basaltic andesite, Basaltic andesites, Caldera, Caldera collapse, Clinopyroxene, Companion plots, Compositional, Concordia university, Contrib, Crustal, Crustal assimilation, Crystal fractionation, Dacite, Dacitic, Felsic, Fractional crystallization, Fractionation, Hyperbolic distributions, Inclusion, Incompatible, Labr, Lalonde, Langmuir, Lava, Linear trend, Mafic, Mafic glass, Mafic liquids, Magma, Magmatic, Major elements, Mineral chemistry, Nisyros, Nisyros lavas, Nisyros volcano, Olivine, Opaque oxides, Orthopyroxene, Oxide, Paola, Parentheses population, Parentheses representative analyses, Pearce, Petrogenetic, Petrol, Phenocrysts, Plagioclase, Plagioclase phenocrysts, Postcaldera dacites, Pumice, Pumiceous, Pyroclastic, Rhyodacite, Rhyodacite flows, Rhyodacites, Rhyolite, Seymour, Silicic, Silicic andesites, Sio2, Source region, Subaerial, Subaerial andesites, Systematics, Tio2, Trace elements, Vlassopoulos, Vlassopoulos table, Volcanic, Volcanic rocks, Volcanism, Volcano, Volcanol, Wyers.
Abstract
Abstract: Rocks of the calc-alkaline volcanic complex of Nisyros, at the eastern end of the Quaternary South Aegean volcanic arc, range in composition from basaltic andesite to rhyodacite. Major- and compatible trace-element systematics are dominated by crystal fractionation, involving olivine, clinopyroxene, plagioclase, and magnetite in the mafic to intermediate compositional range and plagioclase, clinopyroxene, hypersthene, Fe-Ti oxides, and apatite in the intermediate to silicic range, although there is a marked paucity of lavas with 60–66 wt.% SiO2. The occurrence of andesitic inclusions in pre- and post-caldera dacites as well as reversely zoned and/or partly resorbed phenocrysts, exotic mineralogy (e.g., forsteritic olivine), compositionally bimodal plagioclase phenocryst populations, and the observation of two distinct glass phases in melt inclusions and pumices all indicate that magma mixing processes have played a role in the petrogenesis of Nisyros. Incompatible trace-element systematics are consistent with mixing between mafic and silicic end members. Major-element binary mixing calculations between end members successfully reproduce the dacite composition. The eruptive sequence at Nisyros suggests the existence of a compositionally zoned magma chamber, in which mixing between underlying more mafic magma and overlying rhyodacitic melt result in the formation of dacitic magmas. Inherent mineral assemblages in basaltic andesites indicate that mixing between mafic liquids and between mafic and more silicic liquids played also a role in their petrogenesis.
Url:
DOI: 10.1016/0377-0273(92)90097-W
Links to Exploration step
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Major- and compatible trace-element systematics are dominated by crystal fractionation, involving olivine, clinopyroxene, plagioclase, and magnetite in the mafic to intermediate compositional range and plagioclase, clinopyroxene, hypersthene, Fe-Ti oxides, and apatite in the intermediate to silicic range, although there is a marked paucity of lavas with 60–66 wt.% SiO2. The occurrence of andesitic inclusions in pre- and post-caldera dacites as well as reversely zoned and/or partly resorbed phenocrysts, exotic mineralogy (e.g., forsteritic olivine), compositionally bimodal plagioclase phenocryst populations, and the observation of two distinct glass phases in melt inclusions and pumices all indicate that magma mixing processes have played a role in the petrogenesis of Nisyros. Incompatible trace-element systematics are consistent with mixing between mafic and silicic end members. Major-element binary mixing calculations between end members successfully reproduce the dacite composition. The eruptive sequence at Nisyros suggests the existence of a compositionally zoned magma chamber, in which mixing between underlying more mafic magma and overlying rhyodacitic melt result in the formation of dacitic magmas. Inherent mineral assemblages in basaltic andesites indicate that mixing between mafic liquids and between mafic and more silicic liquids played also a role in their petrogenesis.</div></front></TEI><istex><corpusName>elsevier</corpusName><keywords><teeft><json:string>nisyros</json:string><json:string>andesite</json:string><json:string>dacite</json:string><json:string>magma</json:string><json:string>plagioclase</json:string><json:string>mafic</json:string><json:string>basaltic</json:string><json:string>silicic</json:string><json:string>rhyodacite</json:string><json:string>sio2</json:string><json:string>vlassopoulos</json:string><json:string>andesitic</json:string><json:string>subaerial</json:string><json:string>seymour</json:string><json:string>lava</json:string><json:string>olivine</json:string><json:string>clinopyroxene</json:string><json:string>felsic</json:string><json:string>pumice</json:string><json:string>paola</json:string><json:string>petrol</json:string><json:string>phenocrysts</json:string><json:string>wyers</json:string><json:string>basalt</json:string><json:string>nisyros volcano</json:string><json:string>caldera</json:string><json:string>contrib</json:string><json:string>volcanism</json:string><json:string>magmatic</json:string><json:string>apatite</json:string><json:string>petrogenetic</json:string><json:string>pyroclastic</json:string><json:string>dacitic</json:string><json:string>tio2</json:string><json:string>pearce</json:string><json:string>crustal</json:string><json:string>amphibole</json:string><json:string>rhyolite</json:string><json:string>lalonde</json:string><json:string>labr</json:string><json:string>orthopyroxene</json:string><json:string>nisyros lavas</json:string><json:string>langmuir</json:string><json:string>systematics</json:string><json:string>rhyodacites</json:string><json:string>pumiceous</json:string><json:string>crystal fractionation</json:string><json:string>volcanol</json:string><json:string>volcano</json:string><json:string>compositional</json:string><json:string>basaltic andesite</json:string><json:string>volcanic rocks</json:string><json:string>subaerial andesites</json:string><json:string>andesitic inclusions</json:string><json:string>trace elements</json:string><json:string>major elements</json:string><json:string>vlassopoulos table</json:string><json:string>incompatible</json:string><json:string>inclusion</json:string><json:string>basaltic andesites</json:string><json:string>opaque oxides</json:string><json:string>plagioclase phenocrysts</json:string><json:string>mafic liquids</json:string><json:string>fractional crystallization</json:string><json:string>linear trend</json:string><json:string>caldera collapse</json:string><json:string>volcanic</json:string><json:string>oxide</json:string><json:string>concordia university</json:string><json:string>postcaldera dacites</json:string><json:string>silicic andesites</json:string><json:string>crustal assimilation</json:string><json:string>parentheses population</json:string><json:string>rhyodacite flows</json:string><json:string>parentheses representative analyses</json:string><json:string>source region</json:string><json:string>hyperbolic distributions</json:string><json:string>andesite inclusion</json:string><json:string>mafic glass</json:string><json:string>companion plots</json:string><json:string>mineral chemistry</json:string><json:string>fractionation</json:string></teeft></keywords><author><json:item><name>Karen St. Seymour</name><affiliations><json:string>Geology Department, Concordia University, 7141 Sherbrooke St. West, Montreal, Que. H4B 1R6, Canada</json:string></affiliations></json:item><json:item><name>Dimitri Vlassopoulos</name><affiliations><json:string>Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91106, USA</json:string></affiliations></json:item></author><language><json:string>eng</json:string></language><originalGenre><json:string>Full-length article</json:string></originalGenre><abstract>Rocks of the calc-alkaline volcanic complex of Nisyros, at the eastern end of the Quaternary South Aegean volcanic arc, range in composition from basaltic andesite to rhyodacite. Major- and compatible trace-element systematics are dominated by crystal fractionation, involving olivine, clinopyroxene, plagioclase, and magnetite in the mafic to intermediate compositional range and plagioclase, clinopyroxene, hypersthene, Fe-Ti oxides, and apatite in the intermediate to silicic range, although there is a marked paucity of lavas with 60–66 wt.% SiO2. The occurrence of andesitic inclusions in pre- and post-caldera dacites as well as reversely zoned and/or partly resorbed phenocrysts, exotic mineralogy (e.g., forsteritic olivine), compositionally bimodal plagioclase phenocryst populations, and the observation of two distinct glass phases in melt inclusions and pumices all indicate that magma mixing processes have played a role in the petrogenesis of Nisyros. Incompatible trace-element systematics are consistent with mixing between mafic and silicic end members. Major-element binary mixing calculations between end members successfully reproduce the dacite composition. The eruptive sequence at Nisyros suggests the existence of a compositionally zoned magma chamber, in which mixing between underlying more mafic magma and overlying rhyodacitic melt result in the formation of dacitic magmas. Inherent mineral assemblages in basaltic andesites indicate that mixing between mafic liquids and between mafic and more silicic liquids played also a role in their petrogenesis.</abstract><qualityIndicators><score>7.604</score><pdfVersion>1.2</pdfVersion><pdfPageSize>540 x 756 pts</pdfPageSize><refBibsNative>true</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>1581</abstractCharCount><pdfWordCount>7930</pdfWordCount><pdfCharCount>58598</pdfCharCount><pdfPageCount>27</pdfPageCount><abstractWordCount>217</abstractWordCount></qualityIndicators><title>Magma mixing at Nisyros volcano, as inferred from incompatible trace-element systematics</title><pii><json:string>0377-0273(92)90097-W</json:string></pii><genre><json:string>research-article</json:string></genre><serie><title>A summary of theoretical models and their applications</title><language><json:string>unknown</json:string></language><pages><first>41</first><last>47</last></pages></serie><host><title>Journal of Volcanology and Geothermal Research</title><language><json:string>unknown</json:string></language><publicationDate>1992</publicationDate><issn><json:string>0377-0273</json:string></issn><pii><json:string>S0377-0273(00)X0191-6</json:string></pii><volume>50</volume><issue>3</issue><pages><first>273</first><last>299</last></pages><genre><json:string>journal</json:string></genre></host><categories><wos><json:string>science</json:string><json:string>geosciences, multidisciplinary</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>1992</publicationDate><copyrightDate>1992</copyrightDate><doi><json:string>10.1016/0377-0273(92)90097-W</json:string></doi><id>370A9F4E79C3472143C44081362B4BDDC9DE2EE2</id><score>1</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/370A9F4E79C3472143C44081362B4BDDC9DE2EE2/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/370A9F4E79C3472143C44081362B4BDDC9DE2EE2/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/370A9F4E79C3472143C44081362B4BDDC9DE2EE2/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a">Magma mixing at Nisyros volcano, as inferred from incompatible trace-element systematics</title></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>ELSEVIER</publisher><availability><p>ELSEVIER</p></availability><date>1992</date></publicationStmt><notesStmt><note type="content">Section title: Research paper</note></notesStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a">Magma mixing at Nisyros volcano, as inferred from incompatible trace-element systematics</title><author xml:id="author-0000"><persName><forename type="first">Karen</forename><surname>St. Seymour</surname></persName><note type="correspondence"><p>Correspondence to: K. St. Seymour, Geology Department, Concordia University, 7141 Sherbrooke St. West, Montreal, Que. H4B 1R6, Canada.</p></note><affiliation>Geology Department, Concordia University, 7141 Sherbrooke St. West, Montreal, Que. H4B 1R6, Canada</affiliation></author><author xml:id="author-0001"><persName><forename type="first">Dimitri</forename><surname>Vlassopoulos</surname></persName><affiliation>Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91106, USA</affiliation></author><idno type="istex">370A9F4E79C3472143C44081362B4BDDC9DE2EE2</idno><idno type="DOI">10.1016/0377-0273(92)90097-W</idno><idno type="PII">0377-0273(92)90097-W</idno></analytic><monogr><title level="j">Journal of Volcanology and Geothermal Research</title><title level="j" type="abbrev">VOLGEO</title><idno type="pISSN">0377-0273</idno><idno type="PII">S0377-0273(00)X0191-6</idno><imprint><publisher>ELSEVIER</publisher><date type="published" when="1992"></date><biblScope unit="volume">50</biblScope><biblScope unit="issue">3</biblScope><biblScope unit="page" from="273">273</biblScope><biblScope unit="page" to="299">299</biblScope></imprint></monogr></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1992</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Rocks of the calc-alkaline volcanic complex of Nisyros, at the eastern end of the Quaternary South Aegean volcanic arc, range in composition from basaltic andesite to rhyodacite. Major- and compatible trace-element systematics are dominated by crystal fractionation, involving olivine, clinopyroxene, plagioclase, and magnetite in the mafic to intermediate compositional range and plagioclase, clinopyroxene, hypersthene, Fe-Ti oxides, and apatite in the intermediate to silicic range, although there is a marked paucity of lavas with 60–66 wt.% SiO2. The occurrence of andesitic inclusions in pre- and post-caldera dacites as well as reversely zoned and/or partly resorbed phenocrysts, exotic mineralogy (e.g., forsteritic olivine), compositionally bimodal plagioclase phenocryst populations, and the observation of two distinct glass phases in melt inclusions and pumices all indicate that magma mixing processes have played a role in the petrogenesis of Nisyros. Incompatible trace-element systematics are consistent with mixing between mafic and silicic end members. Major-element binary mixing calculations between end members successfully reproduce the dacite composition. The eruptive sequence at Nisyros suggests the existence of a compositionally zoned magma chamber, in which mixing between underlying more mafic magma and overlying rhyodacitic melt result in the formation of dacitic magmas. Inherent mineral assemblages in basaltic andesites indicate that mixing between mafic liquids and between mafic and more silicic liquids played also a role in their petrogenesis.</p></abstract></profileDesc><revisionDesc><change when="1991-08-26">Modified</change><change when="1992">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/370A9F4E79C3472143C44081362B4BDDC9DE2EE2/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>VOLGEO</jid><aid>9290097W</aid><ce:pii>0377-0273(92)90097-W</ce:pii><ce:doi>10.1016/0377-0273(92)90097-W</ce:doi><ce:copyright type="unknown" year="1992"></ce:copyright></item-info><head><ce:dochead><ce:textfn>Research paper</ce:textfn></ce:dochead><ce:title>Magma mixing at Nisyros volcano, as inferred from incompatible trace-element systematics</ce:title><ce:author-group><ce:author><ce:given-name>Karen</ce:given-name><ce:surname>St. Seymour</ce:surname><ce:cross-ref refid="COR1"><ce:sup>∗</ce:sup></ce:cross-ref><ce:cross-ref refid="AFF1"><ce:sup>a</ce:sup></ce:cross-ref></ce:author><ce:author><ce:given-name>Dimitri</ce:given-name><ce:surname>Vlassopoulos</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>Geology Department, Concordia University, 7141 Sherbrooke St. West, Montreal, Que. H4B 1R6, Canada</ce:textfn></ce:affiliation><ce:affiliation id="AFF2"><ce:label>b</ce:label><ce:textfn>Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91106, USA</ce:textfn></ce:affiliation><ce:correspondence id="COR1"><ce:label>∗</ce:label><ce:text>Correspondence to: K. St. Seymour, Geology Department, Concordia University, 7141 Sherbrooke St. West, Montreal, Que. H4B 1R6, Canada.</ce:text></ce:correspondence></ce:author-group><ce:date-received day="4" month="2" year="1991"></ce:date-received><ce:date-revised day="26" month="8" year="1991"></ce:date-revised><ce:date-accepted day="26" month="8" year="1991"></ce:date-accepted><ce:abstract><ce:section-title>Abstract</ce:section-title><ce:abstract-sec><ce:simple-para>Rocks of the calc-alkaline volcanic complex of Nisyros, at the eastern end of the Quaternary South Aegean volcanic arc, range in composition from basaltic andesite to rhyodacite. Major- and compatible trace-element systematics are dominated by crystal fractionation, involving olivine, clinopyroxene, plagioclase, and magnetite in the mafic to intermediate compositional range and plagioclase, clinopyroxene, hypersthene, Fe-Ti oxides, and apatite in the intermediate to silicic range, although there is a marked paucity of lavas with 60–66 wt.% SiO<ce:inf>2</ce:inf>. The occurrence of andesitic inclusions in pre- and post-caldera dacites as well as reversely zoned and/or partly resorbed phenocrysts, exotic mineralogy (e.g., forsteritic olivine), compositionally bimodal plagioclase phenocryst populations, and the observation of two distinct glass phases in melt inclusions and pumices all indicate that magma mixing processes have played a role in the petrogenesis of Nisyros. Incompatible trace-element systematics are consistent with mixing between mafic and silicic end members. Major-element binary mixing calculations between end members successfully reproduce the dacite composition. The eruptive sequence at Nisyros suggests the existence of a compositionally zoned magma chamber, in which mixing between underlying more mafic magma and overlying rhyodacitic melt result in the formation of dacitic magmas. Inherent mineral assemblages in basaltic andesites indicate that mixing between mafic liquids and between mafic and more silicic liquids played also a role in their petrogenesis.</ce:simple-para></ce:abstract-sec></ce:abstract></head></converted-article></istex:document></istex:metadataXml><mods version="3.6"><titleInfo><title>Magma mixing at Nisyros volcano, as inferred from incompatible trace-element systematics</title></titleInfo><titleInfo type="alternative" contentType="CDATA"><title>Magma mixing at Nisyros volcano, as inferred from incompatible trace-element systematics</title></titleInfo><name type="personal"><namePart type="given">Karen</namePart><namePart type="family">St. Seymour</namePart><affiliation>Geology Department, Concordia University, 7141 Sherbrooke St. West, Montreal, Que. H4B 1R6, Canada</affiliation><description>Correspondence to: K. St. Seymour, Geology Department, Concordia University, 7141 Sherbrooke St. West, Montreal, Que. H4B 1R6, Canada.</description><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Dimitri</namePart><namePart type="family">Vlassopoulos</namePart><affiliation>Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91106, USA</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">1992</dateIssued><dateModified encoding="w3cdtf">1991-08-26</dateModified><copyrightDate encoding="w3cdtf">1992</copyrightDate></originInfo><language><languageTerm type="code" authority="iso639-2b">eng</languageTerm><languageTerm type="code" authority="rfc3066">en</languageTerm></language><abstract lang="en">Abstract: Rocks of the calc-alkaline volcanic complex of Nisyros, at the eastern end of the Quaternary South Aegean volcanic arc, range in composition from basaltic andesite to rhyodacite. Major- and compatible trace-element systematics are dominated by crystal fractionation, involving olivine, clinopyroxene, plagioclase, and magnetite in the mafic to intermediate compositional range and plagioclase, clinopyroxene, hypersthene, Fe-Ti oxides, and apatite in the intermediate to silicic range, although there is a marked paucity of lavas with 60–66 wt.% SiO2. The occurrence of andesitic inclusions in pre- and post-caldera dacites as well as reversely zoned and/or partly resorbed phenocrysts, exotic mineralogy (e.g., forsteritic olivine), compositionally bimodal plagioclase phenocryst populations, and the observation of two distinct glass phases in melt inclusions and pumices all indicate that magma mixing processes have played a role in the petrogenesis of Nisyros. Incompatible trace-element systematics are consistent with mixing between mafic and silicic end members. Major-element binary mixing calculations between end members successfully reproduce the dacite composition. The eruptive sequence at Nisyros suggests the existence of a compositionally zoned magma chamber, in which mixing between underlying more mafic magma and overlying rhyodacitic melt result in the formation of dacitic magmas. Inherent mineral assemblages in basaltic andesites indicate that mixing between mafic liquids and between mafic and more silicic liquids played also a role in their petrogenesis.</abstract><note type="content">Section title: Research paper</note><relatedItem type="host"><titleInfo><title>Journal of Volcanology and Geothermal Research</title></titleInfo><titleInfo type="abbreviated"><title>VOLGEO</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">19920430</dateIssued></originInfo><identifier type="ISSN">0377-0273</identifier><identifier type="PII">S0377-0273(00)X0191-6</identifier><part><date>19920430</date><detail type="volume"><number>50</number><caption>vol.</caption></detail><detail type="issue"><number>3</number><caption>no.</caption></detail><extent unit="issue-pages"><start>207</start><end>344</end></extent><extent unit="pages"><start>273</start><end>299</end></extent></part></relatedItem><identifier type="istex">370A9F4E79C3472143C44081362B4BDDC9DE2EE2</identifier><identifier type="ark">ark:/67375/6H6-G5S7VFBD-7</identifier><identifier type="DOI">10.1016/0377-0273(92)90097-W</identifier><identifier type="PII">0377-0273(92)90097-W</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/370A9F4E79C3472143C44081362B4BDDC9DE2EE2/metadata/json</uri></json:item></metadata></istex></record>Pour manipuler ce document sous Unix (Dilib)
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