The origin of iron-rich muds at the Kameni Islands, Santorini, Greece
Identifieur interne : 000470 ( Istex/Corpus ); précédent : 000469; suivant : 000471The origin of iron-rich muds at the Kameni Islands, Santorini, Greece
Auteurs : Kurt Boström ; Lennart WidenfalkSource :
- Chemical Geology [ 0009-2541 ] ; 1984.
English descriptors
- KwdEn :
- Aegean plate, Analytical procedures, Bonatti, Bostrsm, Butuzova, Caldera, Cause deposition, Chemical compositions, Detritus, Dynamic environment, Emission spectrometry, Extensive oxidation, Ferric hydroxide, Geol, Good agreement, High concentrations, Hydrogen sulfide, Hydrostatic head, Hydrothermal, Hydrothermal muds, Hydrothermal processes, Hydrothermal solutions, Hydrothermal system, Kameni, Kameni islands, Kameni muds, Lava, Lexington books, Many trace elements, Metalliferous, Metalliferous solutions, Ocean floor, Other hand, Other metalliferous sediments, Palaea, Palaea kameni, Partial correlations, Pelagic sediments, Previous studies, Puchelt, Regression line, Relative error, Ridge sediments, Rock detritus, Rock interactions, Santorini, Santorini caldera, Santorini rocks, Sediment, Sio2, Solid line, Stockholm contrib, Sulfide, Sulfuric acid, Trace elements, Volcanic sediments.
- Teeft :
- Aegean plate, Analytical procedures, Bonatti, Bostrsm, Butuzova, Caldera, Cause deposition, Chemical compositions, Detritus, Dynamic environment, Emission spectrometry, Extensive oxidation, Ferric hydroxide, Geol, Good agreement, High concentrations, Hydrogen sulfide, Hydrostatic head, Hydrothermal, Hydrothermal muds, Hydrothermal processes, Hydrothermal solutions, Hydrothermal system, Kameni, Kameni islands, Kameni muds, Lava, Lexington books, Many trace elements, Metalliferous, Metalliferous solutions, Ocean floor, Other hand, Other metalliferous sediments, Palaea, Palaea kameni, Partial correlations, Pelagic sediments, Previous studies, Puchelt, Regression line, Relative error, Ridge sediments, Rock detritus, Rock interactions, Santorini, Santorini caldera, Santorini rocks, Sediment, Sio2, Solid line, Stockholm contrib, Sulfide, Sulfuric acid, Trace elements, Volcanic sediments.
Abstract
Abstract: Hydrothermal sediments form in several places within the Santorini caldera. The sediments at the most active hot submarine spring (at SW Nea Kameni) consist of 40–48% Fe2O3 and 8–15% SiO2, but only little Al2O3 (0.5–1.6%), P (0.1–0.3%), Mn (100–450 ppm), Sr, Zr, Ba, Zn and V (∼30–200 ppm) and Cu, Ni and Y (∼ 1–30 ppm) are present.The sediments contain more Fe and P and less Si, Al, Mn and many trace elements than sediments formed at less active springs at Palaea Kameni; the differences probably being caused by faster deposition rates of Fe at Nea Kameni and less dilution by rock detritus, which delivers Al, Si and Mn. The Santorini sediments differ much from other exhalative sediments at present or old spreading centers, for example on the East Pacific Rise, in the Red Sea or at En Kafala, which are rich in Mn, Cu, Zn, Ni and Ba.Hydrothermal rock leaching probably occurs at much lower pH-values at Santorini than on the East Pacific Rise, causing a more complete breakdown of the leached rock at Santorini. The very low trace element to iron ratios in the rocks at Santorini, therefore, prevent the hydrothermal solutions there from being very rich in trace elements.The very acid leaching solutions at Santorini are created by extensive oxidation of hydrogen sulfide to sulfuric acid, a process that is readily possible due to the close proximity of the oxygen-rich atmosphere to the top of the magma chamber.
Url:
DOI: 10.1016/0009-2541(84)90015-9
Links to Exploration step
ISTEX:B04D5735E9453811F5A36134BC7D2EDADA1CDCBALe document en format XML
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muds</term><term>Lava</term><term>Lexington books</term><term>Many trace elements</term><term>Metalliferous</term><term>Metalliferous solutions</term><term>Ocean floor</term><term>Other hand</term><term>Other metalliferous sediments</term><term>Palaea</term><term>Palaea kameni</term><term>Partial correlations</term><term>Pelagic sediments</term><term>Previous studies</term><term>Puchelt</term><term>Regression line</term><term>Relative error</term><term>Ridge sediments</term><term>Rock detritus</term><term>Rock interactions</term><term>Santorini</term><term>Santorini caldera</term><term>Santorini rocks</term><term>Sediment</term><term>Sio2</term><term>Solid line</term><term>Stockholm contrib</term><term>Sulfide</term><term>Sulfuric acid</term><term>Trace elements</term><term>Volcanic sediments</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: Hydrothermal sediments form in 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The sediments at the most active hot submarine spring (at SW Nea Kameni) consist of 40–48% Fe2O3 and 8–15% SiO2, but only little Al2O3 (0.5–1.6%), P (0.1–0.3%), Mn (100–450 ppm), Sr, Zr, Ba, Zn and V (∼30–200 ppm) and Cu, Ni and Y (∼ 1–30 ppm) are present.The sediments contain more Fe and P and less Si, Al, Mn and many trace elements than sediments formed at less active springs at Palaea Kameni; the differences probably being caused by faster deposition rates of Fe at Nea Kameni and less dilution by rock detritus, which delivers Al, Si and Mn. The Santorini sediments differ much from other exhalative sediments at present or old spreading centers, for example on the East Pacific Rise, in the Red Sea or at En Kafala, which are rich in Mn, Cu, Zn, Ni and Ba.Hydrothermal rock leaching probably occurs at much lower pH-values at Santorini than on the East Pacific Rise, causing a more complete breakdown of the leached rock at Santorini. The very low trace element to iron ratios in the rocks at Santorini, therefore, prevent the hydrothermal solutions there from being very rich in trace elements.The very acid leaching solutions at Santorini are created by extensive oxidation of hydrogen sulfide to sulfuric acid, a process that is readily possible due to the close proximity of the oxygen-rich atmosphere to the top of the magma chamber.</div></front></TEI><istex><corpusName>elsevier</corpusName><keywords><teeft><json:string>santorini</json:string><json:string>kameni</json:string><json:string>puchelt</json:string><json:string>bostrsm</json:string><json:string>hydrothermal</json:string><json:string>butuzova</json:string><json:string>geol</json:string><json:string>bonatti</json:string><json:string>metalliferous</json:string><json:string>palaea</json:string><json:string>detritus</json:string><json:string>caldera</json:string><json:string>sio2</json:string><json:string>sediment</json:string><json:string>rock detritus</json:string><json:string>palaea kameni</json:string><json:string>sulfuric acid</json:string><json:string>kameni islands</json:string><json:string>metalliferous solutions</json:string><json:string>regression line</json:string><json:string>sulfide</json:string><json:string>lava</json:string><json:string>analytical procedures</json:string><json:string>santorini rocks</json:string><json:string>many trace elements</json:string><json:string>hydrothermal system</json:string><json:string>stockholm contrib</json:string><json:string>lexington books</json:string><json:string>hydrothermal solutions</json:string><json:string>trace elements</json:string><json:string>chemical compositions</json:string><json:string>other hand</json:string><json:string>other metalliferous sediments</json:string><json:string>relative error</json:string><json:string>emission spectrometry</json:string><json:string>volcanic sediments</json:string><json:string>solid line</json:string><json:string>hydrothermal processes</json:string><json:string>kameni muds</json:string><json:string>extensive oxidation</json:string><json:string>partial correlations</json:string><json:string>cause deposition</json:string><json:string>santorini caldera</json:string><json:string>ferric hydroxide</json:string><json:string>high concentrations</json:string><json:string>good agreement</json:string><json:string>rock interactions</json:string><json:string>hydrogen sulfide</json:string><json:string>hydrostatic head</json:string><json:string>hydrothermal muds</json:string><json:string>ridge sediments</json:string><json:string>aegean plate</json:string><json:string>pelagic sediments</json:string><json:string>dynamic environment</json:string><json:string>ocean floor</json:string><json:string>previous studies</json:string></teeft></keywords><author><json:item><name>Kurt Boström</name><affiliations><json:string>Department of Economic Geology, University of Luleå, S-951 87 Luleå Sweden</json:string></affiliations></json:item><json:item><name>Lennart Widenfalk</name><affiliations><json:string>Department of Economic Geology, University of Luleå, S-951 87 Luleå Sweden</json:string></affiliations></json:item></author><articleId><json:string>84900159</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>Full-length article</json:string></originalGenre><abstract>Hydrothermal sediments form in several places within the Santorini caldera. The sediments at the most active hot submarine spring (at SW Nea Kameni) consist of 40–48% Fe2O3 and 8–15% SiO2, but only little Al2O3 (0.5–1.6%), P (0.1–0.3%), Mn (100–450 ppm), Sr, Zr, Ba, Zn and V (∼30–200 ppm) and Cu, Ni and Y (∼ 1–30 ppm) are present.The sediments contain more Fe and P and less Si, Al, Mn and many trace elements than sediments formed at less active springs at Palaea Kameni; the differences probably being caused by faster deposition rates of Fe at Nea Kameni and less dilution by rock detritus, which delivers Al, Si and Mn. The Santorini sediments differ much from other exhalative sediments at present or old spreading centers, for example on the East Pacific Rise, in the Red Sea or at En Kafala, which are rich in Mn, Cu, Zn, Ni and Ba.Hydrothermal rock leaching probably occurs at much lower pH-values at Santorini than on the East Pacific Rise, causing a more complete breakdown of the leached rock at Santorini. The very low trace element to iron ratios in the rocks at Santorini, therefore, prevent the hydrothermal solutions there from being very rich in trace elements.The very acid leaching solutions at Santorini are created by extensive oxidation of hydrogen sulfide to sulfuric acid, a process that is readily possible due to the close proximity of the oxygen-rich atmosphere to the top of the magma chamber.</abstract><qualityIndicators><score>7.892</score><pdfVersion>1.2</pdfVersion><pdfPageSize>468 x 684 pts</pdfPageSize><refBibsNative>true</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>1423</abstractCharCount><pdfWordCount>6347</pdfWordCount><pdfCharCount>31235</pdfCharCount><pdfPageCount>16</pdfPageCount><abstractWordCount>241</abstractWordCount></qualityIndicators><title>The origin of iron-rich muds at the Kameni Islands, Santorini, Greece</title><pii><json:string>0009-2541(84)90015-9</json:string></pii><genre><json:string>research-article</json:string></genre><serie><title>Progress in Oceanography</title><language><json:string>unknown</json:string></language><volume>Vol. 3</volume><pages><first>7</first><last>22</last></pages></serie><host><title>Chemical Geology</title><language><json:string>unknown</json:string></language><publicationDate>1984</publicationDate><issn><json:string>0009-2541</json:string></issn><pii><json:string>S0009-2541(00)X0141-6</json:string></pii><volume>42</volume><issue>1–4</issue><pages><first>203</first><last>218</last></pages><genre><json:string>journal</json:string></genre></host><categories><wos><json:string>science</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>1984</publicationDate><copyrightDate>1984</copyrightDate><doi><json:string>10.1016/0009-2541(84)90015-9</json:string></doi><id>B04D5735E9453811F5A36134BC7D2EDADA1CDCBA</id><score>1</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/B04D5735E9453811F5A36134BC7D2EDADA1CDCBA/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/B04D5735E9453811F5A36134BC7D2EDADA1CDCBA/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/B04D5735E9453811F5A36134BC7D2EDADA1CDCBA/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">The origin of iron-rich muds at the Kameni Islands, Santorini, Greece</title></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>ELSEVIER</publisher><availability><p>ELSEVIER</p></availability><date>1984</date></publicationStmt><notesStmt><note type="content">Section title: Research paper</note></notesStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">The origin of iron-rich muds at the Kameni Islands, Santorini, Greece</title><author xml:id="author-0000"><persName><forename type="first">Kurt</forename><surname>Boström</surname></persName><note type="biography">Present address: Department of Geology, University of Stockholm, S-106 91 Stockholm, Sweden.</note><affiliation>Present address: Department of Geology, University of Stockholm, S-106 91 Stockholm, Sweden.</affiliation><affiliation>Department of Economic Geology, University of Luleå, S-951 87 Luleå Sweden</affiliation></author><author xml:id="author-0001"><persName><forename type="first">Lennart</forename><surname>Widenfalk</surname></persName><affiliation>Department of Economic Geology, University of Luleå, S-951 87 Luleå Sweden</affiliation></author><idno type="istex">B04D5735E9453811F5A36134BC7D2EDADA1CDCBA</idno><idno type="DOI">10.1016/0009-2541(84)90015-9</idno><idno type="PII">0009-2541(84)90015-9</idno><idno type="ArticleID">84900159</idno></analytic><monogr><title level="j">Chemical Geology</title><title level="j" type="abbrev">CHEMGE</title><idno type="pISSN">0009-2541</idno><idno type="PII">S0009-2541(00)X0141-6</idno><imprint><publisher>ELSEVIER</publisher><date type="published" when="1984"></date><biblScope unit="volume">42</biblScope><biblScope unit="issue">1–4</biblScope><biblScope unit="page" from="203">203</biblScope><biblScope unit="page" to="218">218</biblScope></imprint></monogr></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1984</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Hydrothermal sediments form in several places within the Santorini caldera. The sediments at the most active hot submarine spring (at SW Nea Kameni) consist of 40–48% Fe2O3 and 8–15% SiO2, but only little Al2O3 (0.5–1.6%), P (0.1–0.3%), Mn (100–450 ppm), Sr, Zr, Ba, Zn and V (∼30–200 ppm) and Cu, Ni and Y (∼ 1–30 ppm) are present.The sediments contain more Fe and P and less Si, Al, Mn and many trace elements than sediments formed at less active springs at Palaea Kameni; the differences probably being caused by faster deposition rates of Fe at Nea Kameni and less dilution by rock detritus, which delivers Al, Si and Mn. The Santorini sediments differ much from other exhalative sediments at present or old spreading centers, for example on the East Pacific Rise, in the Red Sea or at En Kafala, which are rich in Mn, Cu, Zn, Ni and Ba.Hydrothermal rock leaching probably occurs at much lower pH-values at Santorini than on the East Pacific Rise, causing a more complete breakdown of the leached rock at Santorini. The very low trace element to iron ratios in the rocks at Santorini, therefore, prevent the hydrothermal solutions there from being very rich in trace elements.The very acid leaching solutions at Santorini are created by extensive oxidation of hydrogen sulfide to sulfuric acid, a process that is readily possible due to the close proximity of the oxygen-rich atmosphere to the top of the magma chamber.</p></abstract></profileDesc><revisionDesc><change when="1983-05-27">Modified</change><change when="1984">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/B04D5735E9453811F5A36134BC7D2EDADA1CDCBA/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" xml:lang="en"><item-info><jid>CHEMGE</jid><aid>84900159</aid><ce:pii>0009-2541(84)90015-9</ce:pii><ce:doi>10.1016/0009-2541(84)90015-9</ce:doi><ce:copyright type="unknown" year="1984"></ce:copyright></item-info><head><ce:dochead><ce:textfn>Research paper</ce:textfn></ce:dochead><ce:title>The origin of iron-rich muds at the Kameni Islands, Santorini, Greece</ce:title><ce:author-group><ce:author><ce:given-name>Kurt</ce:given-name><ce:surname>Boström</ce:surname><ce:cross-ref refid="FN1"><ce:sup loc="post">∗</ce:sup></ce:cross-ref></ce:author><ce:author><ce:given-name>Lennart</ce:given-name><ce:surname>Widenfalk</ce:surname></ce:author><ce:affiliation><ce:textfn>Department of Economic Geology, University of Luleå, S-951 87 Luleå Sweden</ce:textfn></ce:affiliation><ce:footnote id="FN1"><ce:label>∗</ce:label><ce:note-para>Present address: Department of Geology, University of Stockholm, S-106 91 Stockholm, Sweden.</ce:note-para></ce:footnote></ce:author-group><ce:date-received day="29" month="12" year="1982"></ce:date-received><ce:date-revised day="27" month="5" year="1983"></ce:date-revised><ce:date-accepted day="27" month="5" year="1983"></ce:date-accepted><ce:abstract class="author"><ce:section-title>Abstract</ce:section-title><ce:abstract-sec><ce:simple-para view="all" id="simple-para.0010">Hydrothermal sediments form in several places within the Santorini caldera. The sediments at the most active hot submarine spring (at SW Nea Kameni) consist of 40–48% Fe<ce:inf loc="post">2</ce:inf>O<ce:inf loc="post">3</ce:inf> and 8–15% SiO<ce:inf loc="post">2</ce:inf>, but only little Al<ce:inf loc="post">2</ce:inf>O<ce:inf loc="post">3</ce:inf> (0.5–1.6%), P (0.1–0.3%), Mn (100–450 ppm), Sr, Zr, Ba, Zn and V (∼30–200 ppm) and Cu, Ni and Y (∼ 1–30 ppm) are present.</ce:simple-para><ce:simple-para view="all" id="simple-para.0015">The sediments contain more Fe and P and less Si, Al, Mn and many trace elements than sediments formed at less active springs at Palaea Kameni; the differences probably being caused by faster deposition rates of Fe at Nea Kameni and less dilution by rock detritus, which delivers Al, Si and Mn. The Santorini sediments differ much from other exhalative sediments at present or old spreading centers, for example on the East Pacific Rise, in the Red Sea or at En Kafala, which are rich in Mn, Cu, Zn, Ni and Ba.</ce:simple-para><ce:simple-para view="all" id="simple-para.0020">Hydrothermal rock leaching probably occurs at much lower pH-values at Santorini than on the East Pacific Rise, causing a more complete breakdown of the leached rock at Santorini. The very low trace element to iron ratios in the rocks at Santorini, therefore, prevent the hydrothermal solutions there from being very rich in trace elements.</ce:simple-para><ce:simple-para view="all" id="simple-para.0025">The very acid leaching solutions at Santorini are created by extensive oxidation of hydrogen sulfide to sulfuric acid, a process that is readily possible due to the close proximity of the oxygen-rich atmosphere to the top of the magma chamber.</ce:simple-para></ce:abstract-sec></ce:abstract></head></converted-article></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>The origin of iron-rich muds at the Kameni Islands, Santorini, Greece</title></titleInfo><titleInfo type="alternative" lang="en" contentType="CDATA"><title>The origin of iron-rich muds at the Kameni Islands, Santorini, Greece</title></titleInfo><name type="personal"><namePart type="given">Kurt</namePart><namePart type="family">Boström</namePart><affiliation>Department of Economic Geology, University of Luleå, S-951 87 Luleå Sweden</affiliation><description>Present address: Department of Geology, University of Stockholm, S-106 91 Stockholm, Sweden.</description><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Lennart</namePart><namePart type="family">Widenfalk</namePart><affiliation>Department of Economic Geology, University of Luleå, S-951 87 Luleå Sweden</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">1984</dateIssued><dateModified encoding="w3cdtf">1983-05-27</dateModified><copyrightDate encoding="w3cdtf">1984</copyrightDate></originInfo><language><languageTerm type="code" authority="iso639-2b">eng</languageTerm><languageTerm type="code" authority="rfc3066">en</languageTerm></language><abstract lang="en">Abstract: Hydrothermal sediments form in several places within the Santorini caldera. The sediments at the most active hot submarine spring (at SW Nea Kameni) consist of 40–48% Fe2O3 and 8–15% SiO2, but only little Al2O3 (0.5–1.6%), P (0.1–0.3%), Mn (100–450 ppm), Sr, Zr, Ba, Zn and V (∼30–200 ppm) and Cu, Ni and Y (∼ 1–30 ppm) are present.The sediments contain more Fe and P and less Si, Al, Mn and many trace elements than sediments formed at less active springs at Palaea Kameni; the differences probably being caused by faster deposition rates of Fe at Nea Kameni and less dilution by rock detritus, which delivers Al, Si and Mn. The Santorini sediments differ much from other exhalative sediments at present or old spreading centers, for example on the East Pacific Rise, in the Red Sea or at En Kafala, which are rich in Mn, Cu, Zn, Ni and Ba.Hydrothermal rock leaching probably occurs at much lower pH-values at Santorini than on the East Pacific Rise, causing a more complete breakdown of the leached rock at Santorini. The very low trace element to iron ratios in the rocks at Santorini, therefore, prevent the hydrothermal solutions there from being very rich in trace elements.The very acid leaching solutions at Santorini are created by extensive oxidation of hydrogen sulfide to sulfuric acid, a process that is readily possible due to the close proximity of the oxygen-rich atmosphere to the top of the magma chamber.</abstract><note type="content">Section title: Research paper</note><relatedItem type="host"><titleInfo><title>Chemical Geology</title></titleInfo><titleInfo type="abbreviated"><title>CHEMGE</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">198401</dateIssued></originInfo><identifier type="ISSN">0009-2541</identifier><identifier type="PII">S0009-2541(00)X0141-6</identifier><part><date>198401</date><detail type="volume"><number>42</number><caption>vol.</caption></detail><detail type="issue"><number>1–4</number><caption>no.</caption></detail><extent unit="issue-pages"><start>1</start><end>364</end></extent><extent unit="pages"><start>203</start><end>218</end></extent></part></relatedItem><identifier type="istex">B04D5735E9453811F5A36134BC7D2EDADA1CDCBA</identifier><identifier type="ark">ark:/67375/6H6-M1JPP4XR-K</identifier><identifier type="DOI">10.1016/0009-2541(84)90015-9</identifier><identifier type="PII">0009-2541(84)90015-9</identifier><identifier type="ArticleID">84900159</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/B04D5735E9453811F5A36134BC7D2EDADA1CDCBA/metadata/json</uri></json:item></metadata></istex></record>Pour manipuler ce document sous Unix (Dilib)
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