Modelling of natural sources of magnetospheric origin in the interpretation of regional induction studies: A review
Identifieur interne : 000E95 ( Istex/Corpus ); précédent : 000E94; suivant : 000E96Modelling of natural sources of magnetospheric origin in the interpretation of regional induction studies: A review
Auteurs : Marianne MareschalSource :
- Surveys in Geophysics [ 0169-3298 ] ; 1986-09-01.
Abstract
Abstract: Traditional interpretation of regional induction studies relies on the assumption that the external inducing field is quasi-form. My review is devoted to as clear as possible a definition of the limitations of this assumption, which is not always justified. Therefore, I will first systematically describe the actual current systems responsible for induction at high, middle or low-latitudes, and then review the means presently available for taking their localised nature into consideration when interpretating surface electromagnetic data. Realistic source models will be presented for all latitudes.
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DOI: 10.1007/BF01904062
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My review is devoted to as clear as possible a definition of the limitations of this assumption, which is not always justified. Therefore, I will first systematically describe the actual current systems responsible for induction at high, middle or low-latitudes, and then review the means presently available for taking their localised nature into consideration when interpretating surface electromagnetic data. Realistic source models will be presented for all latitudes.</div></front></TEI><istex><corpusName>springer</corpusName><author><json:item><name>Marianne Mareschal</name><affiliations><json:string>Centre Géologique et Géophysique, Université des Sciences et Techniques du Languedoc, 34060, Montpellier, France</json:string></affiliations></json:item></author><articleId><json:string>BF01904062</json:string><json:string>Art3</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>ReviewPaper</json:string></originalGenre><abstract>Abstract: Traditional interpretation of regional induction studies relies on the assumption that the external inducing field is quasi-form. My review is devoted to as clear as possible a definition of the limitations of this assumption, which is not always justified. Therefore, I will first systematically describe the actual current systems responsible for induction at high, middle or low-latitudes, and then review the means presently available for taking their localised nature into consideration when interpretating surface electromagnetic data. Realistic source models will be presented for all latitudes.</abstract><qualityIndicators><score>6.032</score><pdfVersion>1.3</pdfVersion><pdfPageSize>482.28 x 698.28 pts</pdfPageSize><refBibsNative>false</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>612</abstractCharCount><pdfWordCount>13955</pdfWordCount><pdfCharCount>82067</pdfCharCount><pdfPageCount>40</pdfPageCount><abstractWordCount>86</abstractWordCount></qualityIndicators><title>Modelling of natural sources of magnetospheric origin in the interpretation of regional induction studies: A review</title><refBibs><json:item><author><json:item><name>S,I Akasofu</name></json:item></author><host><pages><last>48</last><first>29</first></pages><author></author><title>Magnetospheric Currents</title><publicationDate>1984</publicationDate></host><title>The Magnetospheric Currents: An Introduction</title><publicationDate>1984</publicationDate></json:item><json:item><author><json:item><name>C,W Anderson</name></json:item><json:item><name>L,J Lanzerotti</name></json:item><json:item><name>C,G Maclennan</name></json:item></author><host><volume>3</volume><pages><last>498</last><first>495</first></pages><author></author><title>Geophys. 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Reidel Publishing Company, 1986</p></availability><date>1986</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Modelling of natural sources of magnetospheric origin in the interpretation of regional induction studies: A review</title><author xml:id="author-1"><persName><forename type="first">Marianne</forename><surname>Mareschal</surname></persName><affiliation>Centre Géologique et Géophysique, Université des Sciences et Techniques du Languedoc, 34060, Montpellier, France</affiliation></author></analytic><monogr><title level="j">Surveys in Geophysics</title><title level="j" type="sub">An International Review Journal Covering the Entire Field of Geosciences and Related Areas</title><title level="j" type="abbrev">Surv Geophys</title><idno type="journal-ID">10712</idno><idno type="pISSN">0169-3298</idno><idno type="eISSN">1573-0956</idno><idno type="issue-article-count">5</idno><idno type="volume-issue-count">4</idno><imprint><publisher>Kluwer Academic Publishers</publisher><pubPlace>Dordrecht</pubPlace><date type="published" when="1986-09-01"></date><biblScope unit="volume">8</biblScope><biblScope unit="issue">3</biblScope><biblScope unit="page" from="261">261</biblScope><biblScope unit="page" to="300">300</biblScope></imprint></monogr><idno type="istex">78CD6854C305ADAD375B1F1F74B3FF74CFD63735</idno><idno type="DOI">10.1007/BF01904062</idno><idno type="ArticleID">BF01904062</idno><idno type="ArticleID">Art3</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1986</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Abstract: Traditional interpretation of regional induction studies relies on the assumption that the external inducing field is quasi-form. My review is devoted to as clear as possible a definition of the limitations of this assumption, which is not always justified. Therefore, I will first systematically describe the actual current systems responsible for induction at high, middle or low-latitudes, and then review the means presently available for taking their localised nature into consideration when interpretating surface electromagnetic data. Realistic source models will be presented for all latitudes.</p></abstract><abstract xml:lang="fr"><p>Résumé: Les méthodes géophysiques traditionnelles basées sur l'induction électromagnétique régionale utilisent toutes l'hypothèse de base suivant laquelle le champ externe inducteur est quasi-uniforme. Puisque cette hypothèse n'est pas toujours justifiable, ma revue a pour but de définir ses limites aussi clairement que possible. Pour ce faire, je décrirai d'abord systématiquement les véritables systèmes de courants responsables de l'induction à hautes, moyennes ou basses latitudes, pour passer ensuite aux méthodes permettant de prendre en considération leur étendue limitée lors de l'interprétation d'observations de surface. Des modèles réalistes de sources seront présentés pour toutes latitudes.</p></abstract><textClass><keywords scheme="Journal Subject"><list><head>Geosciences</head><item><term>Geosciences, general</term></item><item><term>Geophysics/Geodesy</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1986-09-01">Published</change><change xml:id="refBibs-istex" who="#ISTEX-API" when="2016-11-22">References added</change><change xml:id="refBibs-istex" who="#ISTEX-API" when="2017-01-20">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/78CD6854C305ADAD375B1F1F74B3FF74CFD63735/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>10712</JournalID><JournalPrintISSN>0169-3298</JournalPrintISSN><JournalElectronicISSN>1573-0956</JournalElectronicISSN><JournalTitle>Surveys in Geophysics</JournalTitle><JournalSubTitle>An International Review Journal Covering the Entire Field of Geosciences and Related Areas</JournalSubTitle><JournalAbbreviatedTitle>Surv Geophys</JournalAbbreviatedTitle><JournalSubjectGroup><JournalSubject Type="Primary">Geosciences</JournalSubject><JournalSubject Type="Secondary">Geosciences, general</JournalSubject><JournalSubject Type="Secondary">Geophysics/Geodesy</JournalSubject></JournalSubjectGroup></JournalInfo><Volume><VolumeInfo VolumeType="Regular" TocLevels="0"><VolumeIDStart>8</VolumeIDStart><VolumeIDEnd>8</VolumeIDEnd><VolumeIssueCount>4</VolumeIssueCount></VolumeInfo><Issue IssueType="Regular"><IssueInfo TocLevels="0"><IssueIDStart>3</IssueIDStart><IssueIDEnd>3</IssueIDEnd><IssueArticleCount>5</IssueArticleCount><IssueHistory><CoverDate><Year>1986</Year><Month>9</Month></CoverDate></IssueHistory><IssueCopyright><CopyrightHolderName>D. Reidel Publishing Company</CopyrightHolderName><CopyrightYear>1986</CopyrightYear></IssueCopyright></IssueInfo><Article ID="Art3"><ArticleInfo Language="En" ArticleType="ReviewPaper" NumberingStyle="Unnumbered" TocLevels="0" ContainsESM="No"><ArticleID>BF01904062</ArticleID><ArticleDOI>10.1007/BF01904062</ArticleDOI><ArticleSequenceNumber>3</ArticleSequenceNumber><ArticleTitle Language="En">Modelling of natural sources of magnetospheric origin in the interpretation of regional induction studies: A review</ArticleTitle><ArticleFirstPage>261</ArticleFirstPage><ArticleLastPage>300</ArticleLastPage><ArticleHistory><RegistrationDate><Year>2005</Year><Month>6</Month><Day>21</Day></RegistrationDate></ArticleHistory><ArticleCopyright><CopyrightHolderName>D. Reidel Publishing Company</CopyrightHolderName><CopyrightYear>1986</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>10712</JournalID><VolumeIDStart>8</VolumeIDStart><VolumeIDEnd>8</VolumeIDEnd><IssueIDStart>3</IssueIDStart><IssueIDEnd>3</IssueIDEnd></ArticleContext></ArticleInfo><ArticleHeader><AuthorGroup><Author AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>Marianne</GivenName><FamilyName>Mareschal</FamilyName></AuthorName></Author><Affiliation ID="Aff1"><OrgDivision>Centre Géologique et Géophysique</OrgDivision><OrgName>Université des Sciences et Techniques du Languedoc</OrgName><OrgAddress><Postcode>34060</Postcode><City>Montpellier</City><Country>France</Country></OrgAddress></Affiliation></AuthorGroup><Abstract ID="Abs1" Language="En"><Heading>Abstract</Heading><Para>Traditional interpretation of regional induction studies relies on the assumption that the external inducing field is quasi-form. My review is devoted to as clear as possible a definition of the limitations of this assumption, which is not always justified. Therefore, I will first systematically describe the actual current systems responsible for induction at high, middle or low-latitudes, and then review the means presently available for taking their localised nature into consideration when interpretating surface electromagnetic data. Realistic source models will be presented for all latitudes.</Para></Abstract><Abstract ID="Abs2" Language="Fr"><Heading>Résumé</Heading><Para>Les méthodes géophysiques traditionnelles basées sur l'induction électromagnétique régionale utilisent toutes l'hypothèse de base suivant laquelle le champ externe inducteur est quasi-uniforme. Puisque cette hypothèse n'est pas toujours justifiable, ma revue a pour but de définir ses limites aussi clairement que possible. Pour ce faire, je décrirai d'abord systématiquement les véritables systèmes de courants responsables de l'induction à hautes, moyennes ou basses latitudes, pour passer ensuite aux méthodes permettant de prendre en considération leur étendue limitée lors de l'interprétation d'observations de surface. Des modèles réalistes de sources seront présentés pour toutes latitudes.</Para></Abstract></ArticleHeader><NoBody></NoBody></Article></Issue></Volume></Journal></Publisher></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Modelling of natural sources of magnetospheric origin in the interpretation of regional induction studies: A review</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Modelling of natural sources of magnetospheric origin in the interpretation of regional induction studies: A review</title></titleInfo><name type="personal"><namePart type="given">Marianne</namePart><namePart type="family">Mareschal</namePart><affiliation>Centre Géologique et Géophysique, Université des Sciences et Techniques du Languedoc, 34060, Montpellier, France</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="review-article" displayLabel="ReviewPaper"></genre><originInfo><publisher>Kluwer Academic Publishers</publisher><place><placeTerm type="text">Dordrecht</placeTerm></place><dateIssued encoding="w3cdtf">1986-09-01</dateIssued><copyrightDate encoding="w3cdtf">1986</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType></physicalDescription><abstract lang="en">Abstract: Traditional interpretation of regional induction studies relies on the assumption that the external inducing field is quasi-form. My review is devoted to as clear as possible a definition of the limitations of this assumption, which is not always justified. Therefore, I will first systematically describe the actual current systems responsible for induction at high, middle or low-latitudes, and then review the means presently available for taking their localised nature into consideration when interpretating surface electromagnetic data. Realistic source models will be presented for all latitudes.</abstract><abstract lang="fr">Résumé: Les méthodes géophysiques traditionnelles basées sur l'induction électromagnétique régionale utilisent toutes l'hypothèse de base suivant laquelle le champ externe inducteur est quasi-uniforme. Puisque cette hypothèse n'est pas toujours justifiable, ma revue a pour but de définir ses limites aussi clairement que possible. Pour ce faire, je décrirai d'abord systématiquement les véritables systèmes de courants responsables de l'induction à hautes, moyennes ou basses latitudes, pour passer ensuite aux méthodes permettant de prendre en considération leur étendue limitée lors de l'interprétation d'observations de surface. Des modèles réalistes de sources seront présentés pour toutes latitudes.</abstract><relatedItem type="host"><titleInfo><title>Surveys in Geophysics</title><subTitle>An International Review Journal Covering the Entire Field of Geosciences and Related Areas</subTitle></titleInfo><titleInfo type="abbreviated"><title>Surv Geophys</title></titleInfo><genre type="journal" displayLabel="Archive Journal"></genre><originInfo><dateIssued encoding="w3cdtf">1986-09-01</dateIssued><copyrightDate encoding="w3cdtf">1986</copyrightDate></originInfo><subject><genre>Geosciences</genre><topic>Geosciences, general</topic><topic>Geophysics/Geodesy</topic></subject><identifier type="ISSN">0169-3298</identifier><identifier type="eISSN">1573-0956</identifier><identifier type="JournalID">10712</identifier><identifier type="IssueArticleCount">5</identifier><identifier type="VolumeIssueCount">4</identifier><part><date>1986</date><detail type="volume"><number>8</number><caption>vol.</caption></detail><detail type="issue"><number>3</number><caption>no.</caption></detail><extent unit="pages"><start>261</start><end>300</end></extent></part><recordInfo><recordOrigin>D. Reidel Publishing Company, 1986</recordOrigin></recordInfo></relatedItem><identifier type="istex">78CD6854C305ADAD375B1F1F74B3FF74CFD63735</identifier><identifier type="DOI">10.1007/BF01904062</identifier><identifier type="ArticleID">BF01904062</identifier><identifier type="ArticleID">Art3</identifier><accessCondition type="use and reproduction" contentType="copyright">D. Reidel Publishing Company, 1986</accessCondition><recordInfo><recordContentSource>SPRINGER</recordContentSource><recordOrigin>D. Reidel Publishing Company, 1986</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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