Morphology of the wadati-benioff zone in the hellenic arc
Identifieur interne : 000168 ( Istex/Corpus ); précédent : 000167; suivant : 000169Morphology of the wadati-benioff zone in the hellenic arc
Auteurs : J. Van K ; V. Hanuš ; C. Christova ; S. SimeonovaSource :
- Journal of Geodynamics [ 0264-3707 ] ; 1987.
English descriptors
- KwdEn :
- Active volcanism, Active volcanoes, Adjacent areas, Aegean area, Aegean region, Aseismic, Average subduction rate, Christova, Earthquake foci, Eastern part, Fracture, Fracture zone, Fracture zones, Hanug, Hellenic subduction zone, Hellenic trench, Lower limit, Maximum depth, Morphology, Overlying wedge, Seismically, Subduction, Subduction zone, Tectonophysics, Trench, Trench axis, Van6k, Vertical sections, Volcanism, Volcano, Western part, Western turkey, Zone.
- Teeft :
- Active volcanism, Active volcanoes, Adjacent areas, Aegean area, Aegean region, Aseismic, Average subduction rate, Christova, Earthquake foci, Eastern part, Fracture, Fracture zone, Fracture zones, Hanug, Hellenic subduction zone, Hellenic trench, Lower limit, Maximum depth, Morphology, Overlying wedge, Seismically, Subduction, Subduction zone, Tectonophysics, Trench, Trench axis, Van6k, Vertical sections, Volcanism, Volcano, Western part, Western turkey, Zone.
Abstract
Abstract: The morphology of the Wadati-Benioff zone in the Hellenic arc was established on the basis of the distribution of 1058 earthquake foci. The subduction zone appears to be composed of two separated parts (western and eastern) terminated by seismically active fracture zones. The existence of an intermediate depth aseismic gap, closely connected with active calc-alkaline volcanism, was confirmed in both parts. The age and the average subduction rate of the present subduction cycle were estimated.
Url:
DOI: 10.1016/0264-3707(87)90059-7
Links to Exploration step
ISTEX:502239C8E355713E93C49389F5E212AE1B5BAC53Le document en format XML
<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title>Morphology of the wadati-benioff zone in the hellenic arc</title><author><name sortKey="Van K, J" sort="Van K, J" uniqKey="Van K J" first="J." last="Van K">J. Van K</name><affiliation><mods:affiliation>Geophysical Institute, Czechosl. Acad. Sci., 14131 Prague, Czechoslovakia</mods:affiliation></affiliation></author><author><name sortKey="Hanus, V" sort="Hanus, V" uniqKey="Hanus V" first="V." last="Hanuš">V. Hanuš</name><affiliation><mods:affiliation>Institute of Geology and Geotechnics, Czechosl. Acad. Sci., 18209 Prague, Czechoslovakia</mods:affiliation></affiliation></author><author><name sortKey="Christova, C" sort="Christova, C" uniqKey="Christova C" first="C." last="Christova">C. Christova</name><affiliation><mods:affiliation>Geophysical Institute, Bulgar. Acad. Sci., 1113 Sofia, Bulgaria</mods:affiliation></affiliation></author><author><name sortKey="Simeonova, S" sort="Simeonova, S" uniqKey="Simeonova S" first="S." last="Simeonova">S. Simeonova</name><affiliation><mods:affiliation>Geophysical Institute, Bulgar. Acad. Sci., 1113 Sofia, Bulgaria</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:502239C8E355713E93C49389F5E212AE1B5BAC53</idno><date when="1987" year="1987">1987</date><idno type="doi">10.1016/0264-3707(87)90059-7</idno><idno type="url">https://api.istex.fr/document/502239C8E355713E93C49389F5E212AE1B5BAC53/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">000168</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">000168</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a">Morphology of the wadati-benioff zone in the hellenic arc</title><author><name sortKey="Van K, J" sort="Van K, J" uniqKey="Van K J" first="J." last="Van K">J. Van K</name><affiliation><mods:affiliation>Geophysical Institute, Czechosl. Acad. Sci., 14131 Prague, Czechoslovakia</mods:affiliation></affiliation></author><author><name sortKey="Hanus, V" sort="Hanus, V" uniqKey="Hanus V" first="V." last="Hanuš">V. Hanuš</name><affiliation><mods:affiliation>Institute of Geology and Geotechnics, Czechosl. Acad. Sci., 18209 Prague, Czechoslovakia</mods:affiliation></affiliation></author><author><name sortKey="Christova, C" sort="Christova, C" uniqKey="Christova C" first="C." last="Christova">C. Christova</name><affiliation><mods:affiliation>Geophysical Institute, Bulgar. Acad. Sci., 1113 Sofia, Bulgaria</mods:affiliation></affiliation></author><author><name sortKey="Simeonova, S" sort="Simeonova, S" uniqKey="Simeonova S" first="S." last="Simeonova">S. Simeonova</name><affiliation><mods:affiliation>Geophysical Institute, Bulgar. Acad. Sci., 1113 Sofia, Bulgaria</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Journal of Geodynamics</title><title level="j" type="abbrev">GEOD</title><idno type="ISSN">0264-3707</idno><imprint><publisher>ELSEVIER</publisher><date type="published" when="1987">1987</date><biblScope unit="volume">8</biblScope><biblScope unit="issue">1</biblScope><biblScope unit="page" from="79">79</biblScope><biblScope unit="page" to="93">93</biblScope></imprint><idno type="ISSN">0264-3707</idno></series></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0264-3707</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Active volcanism</term><term>Active volcanoes</term><term>Adjacent areas</term><term>Aegean area</term><term>Aegean region</term><term>Aseismic</term><term>Average subduction rate</term><term>Christova</term><term>Earthquake foci</term><term>Eastern part</term><term>Fracture</term><term>Fracture zone</term><term>Fracture zones</term><term>Hanug</term><term>Hellenic subduction zone</term><term>Hellenic trench</term><term>Lower limit</term><term>Maximum depth</term><term>Morphology</term><term>Overlying wedge</term><term>Seismically</term><term>Subduction</term><term>Subduction zone</term><term>Tectonophysics</term><term>Trench</term><term>Trench axis</term><term>Van6k</term><term>Vertical sections</term><term>Volcanism</term><term>Volcano</term><term>Western part</term><term>Western turkey</term><term>Zone</term></keywords><keywords scheme="Teeft" xml:lang="en"><term>Active volcanism</term><term>Active volcanoes</term><term>Adjacent areas</term><term>Aegean area</term><term>Aegean region</term><term>Aseismic</term><term>Average subduction rate</term><term>Christova</term><term>Earthquake foci</term><term>Eastern part</term><term>Fracture</term><term>Fracture zone</term><term>Fracture zones</term><term>Hanug</term><term>Hellenic subduction zone</term><term>Hellenic trench</term><term>Lower limit</term><term>Maximum depth</term><term>Morphology</term><term>Overlying wedge</term><term>Seismically</term><term>Subduction</term><term>Subduction zone</term><term>Tectonophysics</term><term>Trench</term><term>Trench axis</term><term>Van6k</term><term>Vertical sections</term><term>Volcanism</term><term>Volcano</term><term>Western part</term><term>Western turkey</term><term>Zone</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: The morphology of the Wadati-Benioff zone in the Hellenic arc was established on the basis of the distribution of 1058 earthquake foci. The subduction zone appears to be composed of two separated parts (western and eastern) terminated by seismically active fracture zones. The existence of an intermediate depth aseismic gap, closely connected with active calc-alkaline volcanism, was confirmed in both parts. The age and the average subduction rate of the present subduction cycle were estimated.</div></front></TEI><istex><corpusName>elsevier</corpusName><keywords><teeft><json:string>subduction</json:string><json:string>subduction zone</json:string><json:string>fracture zones</json:string><json:string>eastern part</json:string><json:string>volcanism</json:string><json:string>fracture</json:string><json:string>aseismic</json:string><json:string>van6k</json:string><json:string>vertical sections</json:string><json:string>western part</json:string><json:string>seismically</json:string><json:string>tectonophysics</json:string><json:string>earthquake foci</json:string><json:string>hanug</json:string><json:string>christova</json:string><json:string>aegean area</json:string><json:string>average subduction rate</json:string><json:string>fracture zone</json:string><json:string>active volcanoes</json:string><json:string>hellenic subduction zone</json:string><json:string>maximum depth</json:string><json:string>lower limit</json:string><json:string>zone</json:string><json:string>morphology</json:string><json:string>volcano</json:string><json:string>active volcanism</json:string><json:string>aegean region</json:string><json:string>trench axis</json:string><json:string>western turkey</json:string><json:string>overlying wedge</json:string><json:string>hellenic trench</json:string><json:string>adjacent areas</json:string><json:string>trench</json:string></teeft></keywords><author><json:item><name>J. Vaněk</name><affiliations><json:string>Geophysical Institute, Czechosl. Acad. Sci., 14131 Prague, Czechoslovakia</json:string></affiliations></json:item><json:item><name>V. Hanuš</name><affiliations><json:string>Institute of Geology and Geotechnics, Czechosl. Acad. Sci., 18209 Prague, Czechoslovakia</json:string></affiliations></json:item><json:item><name>C. Christova</name><affiliations><json:string>Geophysical Institute, Bulgar. Acad. Sci., 1113 Sofia, Bulgaria</json:string></affiliations></json:item><json:item><name>S. Simeonova</name><affiliations><json:string>Geophysical Institute, Bulgar. Acad. Sci., 1113 Sofia, Bulgaria</json:string></affiliations></json:item></author><language><json:string>eng</json:string></language><originalGenre><json:string>Full-length article</json:string></originalGenre><abstract>The morphology of the Wadati-Benioff zone in the Hellenic arc was established on the basis of the distribution of 1058 earthquake foci. The subduction zone appears to be composed of two separated parts (western and eastern) terminated by seismically active fracture zones. The existence of an intermediate depth aseismic gap, closely connected with active calc-alkaline volcanism, was confirmed in both parts. The age and the average subduction rate of the present subduction cycle were estimated.</abstract><qualityIndicators><score>4.437</score><pdfVersion>1.2</pdfVersion><pdfPageSize>468 x 684 pts</pdfPageSize><refBibsNative>true</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>497</abstractCharCount><pdfWordCount>3537</pdfWordCount><pdfCharCount>19937</pdfCharCount><pdfPageCount>15</pdfPageCount><abstractWordCount>75</abstractWordCount></qualityIndicators><title>Morphology of the wadati-benioff zone in the hellenic arc</title><pii><json:string>0264-3707(87)90059-7</json:string></pii><genre><json:string>research-article</json:string></genre><serie><title>The Geological Evolution of the Eastern Mediterranean</title><language><json:string>unknown</json:string></language><pages><first>687</first><last>699</last></pages><editor><json:item><name>J.E. Dixon</name></json:item><json:item><name>A.H.F. robertson</name></json:item></editor></serie><host><title>Journal of Geodynamics</title><language><json:string>unknown</json:string></language><publicationDate>1987</publicationDate><issn><json:string>0264-3707</json:string></issn><pii><json:string>S0264-3707(00)X0058-0</json:string></pii><volume>8</volume><issue>1</issue><pages><first>79</first><last>93</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>1987</publicationDate><copyrightDate>1987</copyrightDate><doi><json:string>10.1016/0264-3707(87)90059-7</json:string></doi><id>502239C8E355713E93C49389F5E212AE1B5BAC53</id><score>1</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/502239C8E355713E93C49389F5E212AE1B5BAC53/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/502239C8E355713E93C49389F5E212AE1B5BAC53/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/502239C8E355713E93C49389F5E212AE1B5BAC53/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a">Morphology of the wadati-benioff zone in the hellenic arc</title></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>ELSEVIER</publisher><availability><p>ELSEVIER</p></availability><date>1987</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a">Morphology of the wadati-benioff zone in the hellenic arc</title><author xml:id="author-0000"><persName><forename type="first">J.</forename><surname>Vaněk</surname></persName><affiliation>Geophysical Institute, Czechosl. Acad. Sci., 14131 Prague, Czechoslovakia</affiliation></author><author xml:id="author-0001"><persName><forename type="first">V.</forename><surname>Hanuš</surname></persName><affiliation>Institute of Geology and Geotechnics, Czechosl. Acad. Sci., 18209 Prague, Czechoslovakia</affiliation></author><author xml:id="author-0002"><persName><forename type="first">C.</forename><surname>Christova</surname></persName><affiliation>Geophysical Institute, Bulgar. Acad. Sci., 1113 Sofia, Bulgaria</affiliation></author><author xml:id="author-0003"><persName><forename type="first">S.</forename><surname>Simeonova</surname></persName><affiliation>Geophysical Institute, Bulgar. Acad. Sci., 1113 Sofia, Bulgaria</affiliation></author><idno type="istex">502239C8E355713E93C49389F5E212AE1B5BAC53</idno><idno type="DOI">10.1016/0264-3707(87)90059-7</idno><idno type="PII">0264-3707(87)90059-7</idno></analytic><monogr><title level="j">Journal of Geodynamics</title><title level="j" type="abbrev">GEOD</title><idno type="pISSN">0264-3707</idno><idno type="PII">S0264-3707(00)X0058-0</idno><imprint><publisher>ELSEVIER</publisher><date type="published" when="1987"></date><biblScope unit="volume">8</biblScope><biblScope unit="issue">1</biblScope><biblScope unit="page" from="79">79</biblScope><biblScope unit="page" to="93">93</biblScope></imprint></monogr></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1987</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>The morphology of the Wadati-Benioff zone in the Hellenic arc was established on the basis of the distribution of 1058 earthquake foci. The subduction zone appears to be composed of two separated parts (western and eastern) terminated by seismically active fracture zones. The existence of an intermediate depth aseismic gap, closely connected with active calc-alkaline volcanism, was confirmed in both parts. The age and the average subduction rate of the present subduction cycle were estimated.</p></abstract></profileDesc><revisionDesc><change when="1987">Published</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/502239C8E355713E93C49389F5E212AE1B5BAC53/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>GEOD</jid><aid>87900597</aid><ce:pii>0264-3707(87)90059-7</ce:pii><ce:doi>10.1016/0264-3707(87)90059-7</ce:doi><ce:copyright type="unknown" year="1987"></ce:copyright></item-info><head><ce:title>Morphology of the wadati-benioff zone in the hellenic arc</ce:title><ce:author-group><ce:author><ce:given-name>J.</ce:given-name><ce:surname>Vaněk</ce:surname><ce:cross-ref refid="AFF1"><ce:sup>1</ce:sup></ce:cross-ref></ce:author><ce:author><ce:given-name>V.</ce:given-name><ce:surname>Hanuš</ce:surname><ce:cross-ref refid="AFF2"><ce:sup>2</ce:sup></ce:cross-ref></ce:author><ce:author><ce:given-name>C.</ce:given-name><ce:surname>Christova</ce:surname><ce:cross-ref refid="AFF3"><ce:sup>3</ce:sup></ce:cross-ref></ce:author><ce:author><ce:given-name>S.</ce:given-name><ce:surname>Simeonova</ce:surname><ce:cross-ref refid="AFF3"><ce:sup>3</ce:sup></ce:cross-ref></ce:author><ce:affiliation id="AFF1"><ce:label>1</ce:label><ce:textfn>Geophysical Institute, Czechosl. Acad. Sci., 14131 Prague, Czechoslovakia</ce:textfn></ce:affiliation><ce:affiliation id="AFF2"><ce:label>2</ce:label><ce:textfn>Institute of Geology and Geotechnics, Czechosl. Acad. Sci., 18209 Prague, Czechoslovakia</ce:textfn></ce:affiliation><ce:affiliation id="AFF3"><ce:label>3</ce:label><ce:textfn>Geophysical Institute, Bulgar. Acad. Sci., 1113 Sofia, Bulgaria</ce:textfn></ce:affiliation></ce:author-group><ce:date-received day="26" month="5" year="1987"></ce:date-received><ce:date-accepted day="2" month="7" year="1987"></ce:date-accepted><ce:abstract><ce:section-title>Abstract</ce:section-title><ce:abstract-sec><ce:simple-para>The morphology of the Wadati-Benioff zone in the Hellenic arc was established on the basis of the distribution of 1058 earthquake foci. The subduction zone appears to be composed of two separated parts (western and eastern) terminated by seismically active fracture zones. The existence of an intermediate depth aseismic gap, closely connected with active calc-alkaline volcanism, was confirmed in both parts. The age and the average subduction rate of the present subduction cycle were estimated.</ce:simple-para></ce:abstract-sec></ce:abstract></head></converted-article></istex:document></istex:metadataXml><mods version="3.6"><titleInfo><title>Morphology of the wadati-benioff zone in the hellenic arc</title></titleInfo><titleInfo type="alternative" contentType="CDATA"><title>Morphology of the wadati-benioff zone in the hellenic arc</title></titleInfo><name type="personal"><namePart type="given">J.</namePart><namePart type="family">Vaněk</namePart><affiliation>Geophysical Institute, Czechosl. Acad. Sci., 14131 Prague, Czechoslovakia</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">V.</namePart><namePart type="family">Hanuš</namePart><affiliation>Institute of Geology and Geotechnics, Czechosl. Acad. Sci., 18209 Prague, Czechoslovakia</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">C.</namePart><namePart type="family">Christova</namePart><affiliation>Geophysical Institute, Bulgar. Acad. Sci., 1113 Sofia, Bulgaria</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">S.</namePart><namePart type="family">Simeonova</namePart><affiliation>Geophysical Institute, Bulgar. Acad. Sci., 1113 Sofia, Bulgaria</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">1987</dateIssued><copyrightDate encoding="w3cdtf">1987</copyrightDate></originInfo><language><languageTerm type="code" authority="iso639-2b">eng</languageTerm><languageTerm type="code" authority="rfc3066">en</languageTerm></language><abstract lang="en">Abstract: The morphology of the Wadati-Benioff zone in the Hellenic arc was established on the basis of the distribution of 1058 earthquake foci. The subduction zone appears to be composed of two separated parts (western and eastern) terminated by seismically active fracture zones. The existence of an intermediate depth aseismic gap, closely connected with active calc-alkaline volcanism, was confirmed in both parts. The age and the average subduction rate of the present subduction cycle were estimated.</abstract><relatedItem type="host"><titleInfo><title>Journal of Geodynamics</title></titleInfo><titleInfo type="abbreviated"><title>GEOD</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">198710</dateIssued></originInfo><identifier type="ISSN">0264-3707</identifier><identifier type="PII">S0264-3707(00)X0058-0</identifier><part><date>198710</date><detail type="volume"><number>8</number><caption>vol.</caption></detail><detail type="issue"><number>1</number><caption>no.</caption></detail><extent unit="issue-pages"><start>1</start><end>93</end></extent><extent unit="pages"><start>79</start><end>93</end></extent></part></relatedItem><identifier type="istex">502239C8E355713E93C49389F5E212AE1B5BAC53</identifier><identifier type="ark">ark:/67375/6H6-HVN28KK2-9</identifier><identifier type="DOI">10.1016/0264-3707(87)90059-7</identifier><identifier type="PII">0264-3707(87)90059-7</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/502239C8E355713E93C49389F5E212AE1B5BAC53/metadata/json</uri></json:item></metadata></istex></record>Pour manipuler ce document sous Unix (Dilib)
EXPLOR_STEP=$WICRI_ROOT/Wicri/Terre/explor/NissirosV1/Data/Istex/Corpus
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 000168 | SxmlIndent | more
Ou
HfdSelect -h $EXPLOR_AREA/Data/Istex/Corpus/biblio.hfd -nk 000168 | SxmlIndent | more
Pour mettre un lien sur cette page dans le réseau Wicri
{{Explor lien
|wiki= Wicri/Terre
|area= NissirosV1
|flux= Istex
|étape= Corpus
|type= RBID
|clé= ISTEX:502239C8E355713E93C49389F5E212AE1B5BAC53
|texte= Morphology of the wadati-benioff zone in the hellenic arc
}}
| This area was generated with Dilib version V0.6.33. |  |