Variation of seismic activity and b -value in the wadati-benioff zone of the hellenic arc
Identifieur interne : 000337 ( Istex/Corpus ); précédent : 000336; suivant : 000338Variation of seismic activity and b -value in the wadati-benioff zone of the hellenic arc
Auteurs : C. Christova ; J. Van KSource :
- Studia Geophysica et Geodaetica [ 0039-3169 ] ; 1990-07-01.
English descriptors
- KwdEn :
- Adjacent areas, Better understanding, Cent confidence limits, Correlation coefficient, Corresponding time intervals, Deep structure, Depth distribution, Depth interval, Depth intervals, Depth range, Different depth distribution, Earthquake frequency, Earthquake phenomena, Eastern flank, Eastern flanks, Eastern part, Flank, Focal depth, Fracture, Fracture zones, Geod, Geoph, Geophys, Geophysical institute, Greater depths, Hellenic, Hellenic subduction zone, Hellenic zone, Intermediate earthquakes, Island arcs, Lower part, Lower parts, Magnitude class, Magnitude classes, Open circles, Outer part, Overlying plate, Present study, Regional catalogue, Seismic, Seismic activity, Seismic properties, Seismicity, Shallow earthquakes, Shocks magnitude range, Significant differences, Small number, Studia geoph, Studio geoph, Studla geoph, Subduction, Subduction zone, Tectonic features, Total number, Upper mantle, Upper parts, Vertical distribution, Wadatibenioff zone, Western flank, Whole bodies, Whole body, Whole subducted body, Zone.
- Teeft :
- Adjacent areas, Better understanding, Cent confidence limits, Correlation coefficient, Corresponding time intervals, Deep structure, Depth distribution, Depth interval, Depth intervals, Depth range, Different depth distribution, Earthquake frequency, Earthquake phenomena, Eastern flank, Eastern flanks, Eastern part, Flank, Focal depth, Fracture, Fracture zones, Geod, Geoph, Geophys, Geophysical institute, Greater depths, Hellenic, Hellenic subduction zone, Hellenic zone, Intermediate earthquakes, Island arcs, Lower part, Lower parts, Magnitude class, Magnitude classes, Open circles, Outer part, Overlying plate, Present study, Regional catalogue, Seismic, Seismic activity, Seismic properties, Seismicity, Shallow earthquakes, Shocks magnitude range, Significant differences, Small number, Studia geoph, Studio geoph, Studla geoph, Subduction, Subduction zone, Tectonic features, Total number, Upper mantle, Upper parts, Vertical distribution, Wadatibenioff zone, Western flank, Whole bodies, Whole body, Whole subducted body, Zone.
Abstract
Summary: The statistics of the vertical distribution of earthquake foci belonging to the Wadati-Benioff zone in the Hellenic arc show that the seismic activity, in terms of the total number of events at a given depth range during the period 1901–82, and b value of the frequency-magnitude relation vary with depth in a specific manner. The seismic activity of the western and eastern flanks of the Wadati-Benioff zone varies with depth in a similar way, whereas the b-value depth variation for these two flanks of the subduction zone does not show such a similarity.
Url:
DOI: 10.1007/BF02295926
Links to Exploration step
ISTEX:28B936748F6582ADCB2521D3D6C49A72A3ADA59ELe document en format XML
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Acad. Sci., Sofia</affiliation></author><author xml:id="author-0001"><persName><forename type="first">J.</forename><surname>Vaněk</surname></persName><affiliation>Geophysical Institute, Czechosl. Acad. Sci., Prague</affiliation></author><idno type="istex">28B936748F6582ADCB2521D3D6C49A72A3ADA59E</idno><idno type="ark">ark:/67375/1BB-2B91JQ9H-8</idno><idno type="DOI">10.1007/BF02295926</idno><idno type="article-id">BF02295926</idno><idno type="article-id">Art2</idno></analytic><monogr><title level="j">Studia Geophysica et Geodaetica</title><title level="j" type="abbrev">Stud Geophys Geod</title><idno type="pISSN">0039-3169</idno><idno type="eISSN">1573-1626</idno><idno type="journal-ID">true</idno><idno type="issue-article-count">12</idno><idno type="volume-issue-count">4</idno><imprint><publisher>Kluwer Academic Publishers</publisher><pubPlace>Dordrecht</pubPlace><date type="published" when="1990-07-01"></date><biblScope unit="volume">34</biblScope><biblScope unit="issue">3</biblScope><biblScope unit="page" from="197">197</biblScope><biblScope unit="page" to="207">207</biblScope></imprint></monogr></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1989-08-22</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Summary: The statistics of the vertical distribution of earthquake foci belonging to the Wadati-Benioff zone in the Hellenic arc show that the seismic activity, in terms of the total number of events at a given depth range during the period 1901–82, and b value of the frequency-magnitude relation vary with depth in a specific manner. The seismic activity of the western and eastern flanks of the Wadati-Benioff zone varies with depth in a similar way, whereas the b-value depth variation for these two flanks of the subduction zone does not show such a similarity.</p></abstract><textClass><keywords scheme="Journal Subject"><list><head>Geosciences</head><item><term>Structural Geology</term></item><item><term>Geophysics/Geodesy</term></item><item><term>Meteorology/Climatology</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1989-08-22">Created</change><change when="1990-07-01">Published</change><change xml:id="refBibs-istex" who="#ISTEX-API" when="2017-10-3">References added</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/28B936748F6582ADCB2521D3D6C49A72A3ADA59E/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Springer, Publisher found" wicri:toSee="no header"><istex:xmlDeclaration>version="1.0" encoding="UTF-8"</istex:xmlDeclaration><istex:docType PUBLIC="-//Springer-Verlag//DTD A++ V2.4//EN" URI="http://devel.springer.de/A++/V2.4/DTD/A++V2.4.dtd" name="istex:docType"></istex:docType><istex:document><Publisher><PublisherInfo><PublisherName>Kluwer Academic Publishers</PublisherName><PublisherLocation>Dordrecht</PublisherLocation></PublisherInfo><Journal><JournalInfo JournalProductType="ArchiveJournal" NumberingStyle="Unnumbered"><JournalID>11200</JournalID><JournalPrintISSN>0039-3169</JournalPrintISSN><JournalElectronicISSN>1573-1626</JournalElectronicISSN><JournalTitle>Studia Geophysica et Geodaetica</JournalTitle><JournalAbbreviatedTitle>Stud Geophys Geod</JournalAbbreviatedTitle><JournalSubjectGroup><JournalSubject Type="Primary">Geosciences</JournalSubject><JournalSubject Type="Secondary">Structural Geology</JournalSubject><JournalSubject Type="Secondary">Geophysics/Geodesy</JournalSubject><JournalSubject Type="Secondary">Meteorology/Climatology</JournalSubject></JournalSubjectGroup></JournalInfo><Volume><VolumeInfo TocLevels="0" VolumeType="Regular"><VolumeIDStart>34</VolumeIDStart><VolumeIDEnd>34</VolumeIDEnd><VolumeIssueCount>4</VolumeIssueCount></VolumeInfo><Issue IssueType="Regular"><IssueInfo TocLevels="0"><IssueIDStart>3</IssueIDStart><IssueIDEnd>3</IssueIDEnd><IssueArticleCount>12</IssueArticleCount><IssueHistory><CoverDate><Year>1990</Year><Month>7</Month></CoverDate></IssueHistory><IssueCopyright><CopyrightHolderName>Academia, Publishing House of the Czechoslovak Academy of Sciences</CopyrightHolderName><CopyrightYear>1990</CopyrightYear></IssueCopyright></IssueInfo><Article ID="Art2"><ArticleInfo ArticleType="OriginalPaper" ContainsESM="No" Language="En" NumberingStyle="Unnumbered" TocLevels="0"><ArticleID>BF02295926</ArticleID><ArticleDOI>10.1007/BF02295926</ArticleDOI><ArticleSequenceNumber>2</ArticleSequenceNumber><ArticleTitle Language="En">Variation of seismic activity and<Emphasis Type="Italic">b</Emphasis>-value in the wadati-benioff zone of the hellenic arc</ArticleTitle><ArticleFirstPage>197</ArticleFirstPage><ArticleLastPage>207</ArticleLastPage><ArticleHistory><RegistrationDate><Year>2005</Year><Month>12</Month><Day>30</Day></RegistrationDate><Received><Year>1989</Year><Month>8</Month><Day>22</Day></Received></ArticleHistory><ArticleCopyright><CopyrightHolderName>Academia, Publishing House of the Czechoslovak Academy of Sciences</CopyrightHolderName><CopyrightYear>1990</CopyrightYear></ArticleCopyright><ArticleGrants Type="Regular"><MetadataGrant Grant="OpenAccess"></MetadataGrant><AbstractGrant Grant="OpenAccess"></AbstractGrant><BodyPDFGrant Grant="Restricted"></BodyPDFGrant><BodyHTMLGrant Grant="Restricted"></BodyHTMLGrant><BibliographyGrant Grant="Restricted"></BibliographyGrant><ESMGrant Grant="Restricted"></ESMGrant></ArticleGrants><ArticleContext><JournalID>11200</JournalID><VolumeIDStart>34</VolumeIDStart><VolumeIDEnd>34</VolumeIDEnd><IssueIDStart>3</IssueIDStart><IssueIDEnd>3</IssueIDEnd></ArticleContext></ArticleInfo><ArticleHeader><AuthorGroup><Author AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>C.</GivenName><FamilyName>Christova</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff2"><AuthorName DisplayOrder="Western"><GivenName>J.</GivenName><FamilyName>Vaněk</FamilyName></AuthorName></Author><Affiliation ID="Aff1"><OrgName>Geophysical Institute, Bulgar. Acad. Sci.</OrgName><OrgAddress><City>Sofia</City></OrgAddress></Affiliation><Affiliation ID="Aff2"><OrgName>Geophysical Institute, Czechosl. Acad. Sci.</OrgName><OrgAddress><City>Prague</City></OrgAddress></Affiliation></AuthorGroup><Abstract ID="Abs1" Language="En"><Heading>Summary</Heading><Para>The statistics of the vertical distribution of earthquake foci belonging to the Wadati-Benioff zone in the Hellenic arc show that the seismic activity, in terms of the total number of events at a given depth range during the period 1901–82, and b value of the frequency-magnitude relation vary with depth in a specific manner. The seismic activity of the western and eastern flanks of the Wadati-Benioff zone varies with depth in a similar way, whereas the b-value depth variation for these two flanks of the subduction zone does not show such a similarity.</Para></Abstract></ArticleHeader><NoBody></NoBody></Article></Issue></Volume></Journal></Publisher></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Variation of seismic activity and b -value in the wadati-benioff zone of the hellenic arc</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Variation of seismic activity andb-value in the wadati-benioff zone of the hellenic arc</title></titleInfo><name type="personal"><namePart type="given">C.</namePart><namePart type="family">Christova</namePart><affiliation>Geophysical Institute, Bulgar. Acad. Sci., Sofia</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">J.</namePart><namePart type="family">Vaněk</namePart><affiliation>Geophysical Institute, Czechosl. Acad. Sci., Prague</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="OriginalPaper" 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>Kluwer Academic Publishers</publisher><place><placeTerm type="text">Dordrecht</placeTerm></place><dateCreated encoding="w3cdtf">1989-08-22</dateCreated><dateIssued encoding="w3cdtf">1990-07-01</dateIssued><dateIssued encoding="w3cdtf">1990</dateIssued><copyrightDate encoding="w3cdtf">1990</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><abstract lang="en">Summary: The statistics of the vertical distribution of earthquake foci belonging to the Wadati-Benioff zone in the Hellenic arc show that the seismic activity, in terms of the total number of events at a given depth range during the period 1901–82, and b value of the frequency-magnitude relation vary with depth in a specific manner. The seismic activity of the western and eastern flanks of the Wadati-Benioff zone varies with depth in a similar way, whereas the b-value depth variation for these two flanks of the subduction zone does not show such a similarity.</abstract><relatedItem type="host"><titleInfo><title>Studia Geophysica et Geodaetica</title></titleInfo><titleInfo type="abbreviated"><title>Stud Geophys Geod</title></titleInfo><genre type="journal" displayLabel="Archive Journal" authority="ISTEX" valueURI="https://publication-type.data.istex.fr/ark:/67375/JMC-0GLKJH51-B">journal</genre><originInfo><publisher>Springer</publisher><dateIssued encoding="w3cdtf">1990-07-01</dateIssued><copyrightDate encoding="w3cdtf">1990</copyrightDate></originInfo><subject><genre>Geosciences</genre><topic>Structural Geology</topic><topic>Geophysics/Geodesy</topic><topic>Meteorology/Climatology</topic></subject><identifier type="ISSN">0039-3169</identifier><identifier type="eISSN">1573-1626</identifier><identifier type="JournalID">11200</identifier><identifier type="IssueArticleCount">12</identifier><identifier type="VolumeIssueCount">4</identifier><part><date>1990</date><detail type="volume"><number>34</number><caption>vol.</caption></detail><detail type="issue"><number>3</number><caption>no.</caption></detail><extent unit="pages"><start>197</start><end>207</end></extent></part><recordInfo><recordOrigin>Academia, Publishing House of the Czechoslovak Academy of Sciences, 1990</recordOrigin></recordInfo></relatedItem><identifier type="istex">28B936748F6582ADCB2521D3D6C49A72A3ADA59E</identifier><identifier type="ark">ark:/67375/1BB-2B91JQ9H-8</identifier><identifier type="DOI">10.1007/BF02295926</identifier><identifier type="ArticleID">BF02295926</identifier><identifier type="ArticleID">Art2</identifier><accessCondition type="use and reproduction" contentType="copyright">Academia, Publishing House of the Czechoslovak Academy of Sciences, 1990</accessCondition><recordInfo><recordContentSource authority="ISTEX" authorityURI="https://loaded-corpus.data.istex.fr" valueURI="https://loaded-corpus.data.istex.fr/ark:/67375/XBH-3XSW68JL-F">springer</recordContentSource><recordOrigin>Academia, Publishing House of the Czechoslovak Academy of Sciences, 1990</recordOrigin></recordInfo></mods><json:item><extension>json</extension><original>false</original><mimetype>application/json</mimetype><uri>https://api.istex.fr/document/28B936748F6582ADCB2521D3D6C49A72A3ADA59E/metadata/json</uri></json:item></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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