Palaeomagnetic investigations of the tertiary and quaternary igneous rocks: VIII a palaeomagnetic and petrologic study of volcanics of the valley of Mexico
Identifieur interne : 001140 ( Istex/Corpus ); précédent : 001139; suivant : 001141Palaeomagnetic investigations of the tertiary and quaternary igneous rocks: VIII a palaeomagnetic and petrologic study of volcanics of the valley of Mexico
Auteurs : Freddie Mooser ; Alan E. M. Nairn ; Jörg F. W. NegendankSource :
- Geologische Rundschau [ 0016-7835 ] ; 1974-07-01.
Abstract
Zusammenfassung: Das Becken von Mexiko befindet sich im Zentrum des Transmexikanischen Vulkangürtels, einer Ost-West-Struktur, die den nordamerikanischen Kontinent entlang des 19. Breitengrades durchschneidet. Paläomagnetische Messungen legen die Vermutung nahe, daß 2 (Guadalupe- und Chichinautzin-Gruppe) der 7 vulkanischen Phasen, die das Becken formten, von wahrscheinlich kurzer Dauer waren. Die Chichinautzin-Gruppe, die das Becken im Süden abschnürte, muß sich grundsätzlich in den letzten 700 000 Jahren gebildet haben. Die vulkanische Tätigkeit, die im Oligozän begann und sich kontinuierlich bis in dic heutige Zeit fortsetzte, förderte nachweislich im wesentlichen andesitische Produkte.
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DOI: 10.1007/BF01820824
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ISTEX:3EEA6FC2E3A41D97072D6C2366A74497AE27EA84Le document en format XML
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W." last="Negendank">Jörg F. W. Negendank</name><affiliation><mods:affiliation>Abt. Geowissenschaftliches Laboratorium der Fachgruppe Geographie der Universität Trier-Kaiserslautern, D-55 Trier, Schneidershof, W-Germany</mods:affiliation></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:3EEA6FC2E3A41D97072D6C2366A74497AE27EA84</idno><date when="1974" year="1974">1974</date><idno type="doi">10.1007/BF01820824</idno><idno type="url">https://api.istex.fr/document/3EEA6FC2E3A41D97072D6C2366A74497AE27EA84/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">001140</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">001140</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Palaeomagnetic investigations of the tertiary and quaternary igneous rocks: VIII a palaeomagnetic and petrologic study of volcanics of the valley of Mexico</title><author><name sortKey="Mooser, Freddie" sort="Mooser, Freddie" uniqKey="Mooser F" first="Freddie" last="Mooser">Freddie Mooser</name><affiliation><mods:affiliation>Instituto de Geofisica, Universidad Nacional Autonoina, Torre de Ciencias, Ciudad Universitaria, Mexico 20 D. F., Mexico</mods:affiliation></affiliation></author><author><name sortKey="Nairn, Alan E M" sort="Nairn, Alan E M" uniqKey="Nairn A" first="Alan E. M." last="Nairn">Alan E. M. Nairn</name><affiliation><mods:affiliation>Department of Geology, University of South Carolina, 29208, Columbia, S.C., USA</mods:affiliation></affiliation></author><author><name sortKey="Negendank, Jorg F W" sort="Negendank, Jorg F W" uniqKey="Negendank J" first="Jörg F. W." last="Negendank">Jörg F. W. Negendank</name><affiliation><mods:affiliation>Abt. Geowissenschaftliches Laboratorium der Fachgruppe Geographie der Universität Trier-Kaiserslautern, D-55 Trier, Schneidershof, W-Germany</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Geologische Rundschau</title><title level="j" type="abbrev">Geol Rundsch</title><idno type="ISSN">0016-7835</idno><idno type="eISSN">1432-1149</idno><imprint><publisher>Springer-Verlag</publisher><pubPlace>Berlin/Heidelberg</pubPlace><date type="published" when="1974-07-01">1974-07-01</date><biblScope unit="volume">63</biblScope><biblScope unit="issue">2</biblScope><biblScope unit="page" from="451">451</biblScope><biblScope unit="page" to="483">483</biblScope></imprint><idno type="ISSN">0016-7835</idno></series><idno type="istex">3EEA6FC2E3A41D97072D6C2366A74497AE27EA84</idno><idno type="DOI">10.1007/BF01820824</idno><idno type="ArticleID">BF01820824</idno><idno type="ArticleID">Art4</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0016-7835</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="de">Zusammenfassung: Das Becken von Mexiko befindet sich im Zentrum des Transmexikanischen Vulkangürtels, einer Ost-West-Struktur, die den nordamerikanischen Kontinent entlang des 19. Breitengrades durchschneidet. Paläomagnetische Messungen legen die Vermutung nahe, daß 2 (Guadalupe- und Chichinautzin-Gruppe) der 7 vulkanischen Phasen, die das Becken formten, von wahrscheinlich kurzer Dauer waren. Die Chichinautzin-Gruppe, die das Becken im Süden abschnürte, muß sich grundsätzlich in den letzten 700 000 Jahren gebildet haben. Die vulkanische Tätigkeit, die im Oligozän begann und sich kontinuierlich bis in dic heutige Zeit fortsetzte, förderte nachweislich im wesentlichen andesitische Produkte.</div></front></TEI><istex><corpusName>springer</corpusName><author><json:item><name>Prof. Ing. Freddie Mooser</name><affiliations><json:string>Instituto de Geofisica, Universidad Nacional Autonoina, Torre de Ciencias, Ciudad Universitaria, Mexico 20 D. F., Mexico</json:string></affiliations></json:item><json:item><name>Prof. Dr. Alan E. M. Nairn</name><affiliations><json:string>Department of Geology, University of South Carolina, 29208, Columbia, S.C., USA</json:string></affiliations></json:item><json:item><name>Dr. Jörg F. W. Negendank</name><affiliations><json:string>Abt. Geowissenschaftliches Laboratorium der Fachgruppe Geographie der Universität Trier-Kaiserslautern, D-55 Trier, Schneidershof, W-Germany</json:string></affiliations></json:item></author><articleId><json:string>BF01820824</json:string><json:string>Art4</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>OriginalPaper</json:string></originalGenre><abstract>Abstract: The basin of Mexico lies in the center of the Trans-Mexican Volcanic Belt, an east-west structure which dissects the North American Continent along the 19th parallel. Paleomagnetic measurements suggest that two of the seven eruptive phases —Guadalupe Group and Chichinautzin Group — that formed the basin, probably were of short duration; the Chichinautzin Group, which finally closed the basin to the south, must have been formed principally in the last 700,000 years. The volcanic activity which began in Oligocene time and has continued until the present, has been proved to be essentially andesitic in composition.</abstract><qualityIndicators><score>6.056</score><pdfVersion>1.3</pdfVersion><pdfPageSize>432 x 648 pts</pdfPageSize><refBibsNative>false</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>698</abstractCharCount><pdfWordCount>8931</pdfWordCount><pdfCharCount>54671</pdfCharCount><pdfPageCount>33</pdfPageCount><abstractWordCount>88</abstractWordCount></qualityIndicators><title>Palaeomagnetic investigations of the tertiary and quaternary igneous rocks: VIII a palaeomagnetic and petrologic study of volcanics of the valley of Mexico</title><refBibs><json:item><author><json:item><name>~ ~e</name></json:item><json:item><name>~,~ ~0~ ~-~ ~~ '~ ; _ ~ ~c~ O O ~ ~</name></json:item><json:item><name>~,F Bibliography</name></json:item><json:item><name>Ade-Hall </name></json:item><json:item><name>J,M Khan</name></json:item><json:item><name>M,A Dagley</name></json:item><json:item><name>P Wilson</name></json:item><json:item><name>R,L </name></json:item></author><host><volume>16</volume><pages><last>888</last><first>875</first></pages><author></author><title>MoosE~ et ah --Palaeomagnetic Investigations Further thanks is given to Mr. E. LUTZ</title><publicationDate>1968</publicationDate></host><title>Trier, for drawing some maps, and Mrs. E. KNAPP, Trier, for retyping the manuscript after the incorporation of the newest available data clone in June 1978 in Mexico City. The Deutsche Forschungsgemeinschaft supported these investigations by a grant for oremineralogical equipment A Detailed Opaque Petrological and Magnetic Investigation of a Single Tertiary Lava Flow from Skye, Scotland --I. Iron-Titanium Oxide Petrology</title><publicationDate>1968</publicationDate></json:item><json:item><author><json:item><name>Gunn </name></json:item><json:item><name>B,M Moosell</name></json:item><json:item><name>F </name></json:item></author><host><volume>2</volume><pages><last>616</last><first>577</first></pages><author></author><title>Geochemistry of the Volcanics of Central Mexico. --Bull. 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Mexico</title><publicationDate>1968</publicationDate></host><title>Geologia de la Sierra de Guadalupe</title><publicationDate>1968</publicationDate></json:item><json:item><author><json:item><name>Menaiid </name></json:item><json:item><name>H,W </name></json:item></author><host><volume>66</volume><pages><last>1198</last><first>1149</first></pages><author></author><title>North America. --Bull. Geol. Soc. America</title><publicationDate>1955</publicationDate></host><title>Deformation of the northeastern Pacific Basin and the West Coast of</title><publicationDate>1955</publicationDate></json:item><json:item><author><json:item><name>F Mooser</name></json:item></author><host><pages><last>245</last><first>289</first></pages><author></author><title>The Mexican Volcanic Belt-Structure and Development. Formation of Fractures by Differential Crustal Heating. -Pan American Syn~posium on the Upper Mantle, II Mex. de Suelos The Mexican Volcanic Belt. 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An. del Inst</title><publicationDate>1967</publicationDate></host></json:item><json:item><author><json:item><name>F Mooser</name></json:item><json:item><name>H Meyer-Amc~</name></json:item><json:item><name>A,R Mcbmney</name></json:item></author><host><pages><first>146</first></pages><author></author><title>Catalogue of the active volcanoes of the World</title><publicationDate>1958</publicationDate></host><publicationDate>1958</publicationDate></json:item><json:item><author><json:item><name>Neg~nd </name></json:item><json:item><name>~> </name></json:item><json:item><name>J,F W </name></json:item></author><host><pages><last>20</last><first>308</first></pages><author></author><title>Proceedings of the Mexican Symposium on Geodynamics. --(ILl press.) --: Some aspects of volkanic rocks of the Valley of Mexico</title><publicationDate>1972</publicationDate></host><title>Voleanics of the Valley of Mexico, Part I: Petrography of the volcanies --: Volcanies of the Valley of Mexico, Part II: The Opaque Mineralogy Miinster 197g. -: Stone aspects of volcanic rocks of the Valley of Mexico</title><publicationDate>1972</publicationDate></json:item><json:item><author><json:item><name>Steele </name></json:item><json:item><name>W,K </name></json:item></author><host><volume>11</volume><pages><last>218</last><first>211</first></pages><author></author><title>Mexico. -- Earth Planet. Sci. Letters</title><publicationDate>1971</publicationDate></host><title>Palaeomagnetie directions from the Iztaecihuatl Volcano</title><publicationDate>1971</publicationDate></json:item><json:item><host><pages><last>1044</last><first>1019</first></pages><author><json:item><name>J,H Stewar: R</name></json:item></author><title>Basin and Range Structure: A system of horsts and grabens produced by deep-seated extension</title><publicationDate>1971</publicationDate></host></json:item><json:item><author><json:item><name>Wilson </name></json:item><json:item><name>R,L Hacgerty</name></json:item><json:item><name>S,E Watklxs</name></json:item><json:item><name>N,D </name></json:item></author><host><volume>16</volume><pages><last>96</last><first>79</first></pages><author></author><title>J. R. astr. Soc</title><publicationDate>1968</publicationDate></host><title>Variation of Palaeomagnetie Stability and Other Parameters in a Vertical Traverse of a Single Icelandic Lava. -- Geophys</title><publicationDate>1968</publicationDate></json:item></refBibs><genre><json:string>research-article</json:string></genre><host><volume>63</volume><pages><last>483</last><first>451</first></pages><issn><json:string>0016-7835</json:string></issn><issue>2</issue><subject><json:item><value>Geology</value></json:item><json:item><value>Geophysics/Geodesy</value></json:item></subject><journalId><json:string>531</json:string></journalId><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1432-1149</json:string></eissn><title>Geologische Rundschau</title><publicationDate>1974</publicationDate><copyrightDate>1974</copyrightDate></host><categories><wos></wos><scienceMetrix><json:string>natural sciences</json:string><json:string>earth & environmental sciences</json:string><json:string>geology</json:string></scienceMetrix></categories><publicationDate>1974</publicationDate><copyrightDate>1974</copyrightDate><doi><json:string>10.1007/BF01820824</json:string></doi><id>3EEA6FC2E3A41D97072D6C2366A74497AE27EA84</id><score>0.31312615</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/3EEA6FC2E3A41D97072D6C2366A74497AE27EA84/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/3EEA6FC2E3A41D97072D6C2366A74497AE27EA84/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/3EEA6FC2E3A41D97072D6C2366A74497AE27EA84/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">Palaeomagnetic investigations of the tertiary and quaternary igneous rocks: VIII a palaeomagnetic and petrologic study of volcanics of the valley of Mexico</title><respStmt><resp>Références bibliographiques récupérées via GROBID</resp><name resp="ISTEX-API">ISTEX-API (INIST-CNRS)</name></respStmt><respStmt><resp>Références bibliographiques récupérées via GROBID</resp><name resp="ISTEX-API">ISTEX-API (INIST-CNRS)</name></respStmt></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>Springer-Verlag</publisher><pubPlace>Berlin/Heidelberg</pubPlace><availability><p>Ferdinand Enke Verlag Stuttgart, 1974</p></availability><date>1974</date></publicationStmt><notesStmt><note>Aufsätze</note></notesStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Palaeomagnetic investigations of the tertiary and quaternary igneous rocks: VIII a palaeomagnetic and petrologic study of volcanics of the valley of Mexico</title><author xml:id="author-1"><persName><forename type="first">Freddie</forename><surname>Mooser</surname></persName><roleName type="degree">Prof. Ing.</roleName><affiliation>Instituto de Geofisica, Universidad Nacional Autonoina, Torre de Ciencias, Ciudad Universitaria, Mexico 20 D. F., Mexico</affiliation></author><author xml:id="author-2"><persName><forename type="first">Alan</forename><surname>Nairn</surname></persName><roleName type="degree">Prof. Dr.</roleName><affiliation>Department of Geology, University of South Carolina, 29208, Columbia, S.C., USA</affiliation></author><author xml:id="author-3"><persName><forename type="first">Jörg</forename><surname>Negendank</surname></persName><roleName type="degree">Dr.</roleName><affiliation>Abt. Geowissenschaftliches Laboratorium der Fachgruppe Geographie der Universität Trier-Kaiserslautern, D-55 Trier, Schneidershof, W-Germany</affiliation></author></analytic><monogr><title level="j">Geologische Rundschau</title><title level="j" type="abbrev">Geol Rundsch</title><idno type="journal-ID">531</idno><idno type="pISSN">0016-7835</idno><idno type="eISSN">1432-1149</idno><idno type="issue-article-count">24</idno><idno type="volume-issue-count">3</idno><imprint><publisher>Springer-Verlag</publisher><pubPlace>Berlin/Heidelberg</pubPlace><date type="published" when="1974-07-01"></date><biblScope unit="volume">63</biblScope><biblScope unit="issue">2</biblScope><biblScope unit="page" from="451">451</biblScope><biblScope unit="page" to="483">483</biblScope></imprint></monogr><idno type="istex">3EEA6FC2E3A41D97072D6C2366A74497AE27EA84</idno><idno type="DOI">10.1007/BF01820824</idno><idno type="ArticleID">BF01820824</idno><idno type="ArticleID">Art4</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1974</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="de"><p>Zusammenfassung: Das Becken von Mexiko befindet sich im Zentrum des Transmexikanischen Vulkangürtels, einer Ost-West-Struktur, die den nordamerikanischen Kontinent entlang des 19. Breitengrades durchschneidet. Paläomagnetische Messungen legen die Vermutung nahe, daß 2 (Guadalupe- und Chichinautzin-Gruppe) der 7 vulkanischen Phasen, die das Becken formten, von wahrscheinlich kurzer Dauer waren. Die Chichinautzin-Gruppe, die das Becken im Süden abschnürte, muß sich grundsätzlich in den letzten 700 000 Jahren gebildet haben. Die vulkanische Tätigkeit, die im Oligozän begann und sich kontinuierlich bis in dic heutige Zeit fortsetzte, förderte nachweislich im wesentlichen andesitische Produkte.</p></abstract><abstract xml:lang="en"><p>Abstract: The basin of Mexico lies in the center of the Trans-Mexican Volcanic Belt, an east-west structure which dissects the North American Continent along the 19th parallel. Paleomagnetic measurements suggest that two of the seven eruptive phases —Guadalupe Group and Chichinautzin Group — that formed the basin, probably were of short duration; the Chichinautzin Group, which finally closed the basin to the south, must have been formed principally in the last 700,000 years. The volcanic activity which began in Oligocene time and has continued until the present, has been proved to be essentially andesitic in composition.</p></abstract><abstract xml:lang="fr"><p>Résumé: Le bassin de Mexico se trouve au centre de la ceinture volcanique de Mexico, une structure est-ouest qui recoupe le continent nord-Americain près du 19e parallèle. Les mesures paléomagnétiques conduisent à supposer que deux des sept phases d'activités volcaniques, celles de la Guadaloupe et du Chichinautzin, étaient courtes. Les roches du Groupe de Chichinautzin, fermant le bassin au sud, ont été formées pendant les derniers 700,000 ans. L'activité volcanique, qui a débuté à l'Oligocène et se continue encore actuellement a une charactère essentiellement andésitique.</p></abstract><abstract xml:lang="--"><p>Краткое содержание: Мексиканский бассей н находится в центре трансмексиканского вулканического пояса — некой структу ры, которая пересекае т северо-американский материк вдоль 19-й параллели с во стока на запад. Палеомагнитные изме рения разрешают пола гать, что две из семи вулканически х фаз, именно группа Guadalupe и Chichinautzin, образовавших этот бассейн, повсей вероя тности, были очень непродолжттельными. Группа Chichinautzin, продукты которой сос тавляют границу басс ейна на юге, появилась в последние 700000 лет. Вулканическая деяте льность, начавшаяся в олигоцене и продолжающаяся непрерывно по сегодн я, подняла главным обр азом андезиты.</p></abstract><textClass><keywords scheme="Journal Subject"><list><head>Geosciences</head><item><term>Geology</term></item><item><term>Geophysics/Geodesy</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1974-07-01">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/3EEA6FC2E3A41D97072D6C2366A74497AE27EA84/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>Springer-Verlag</PublisherName><PublisherLocation>Berlin/Heidelberg</PublisherLocation></PublisherInfo><Journal><JournalInfo JournalProductType="ArchiveJournal" NumberingStyle="Unnumbered"><JournalID>531</JournalID><JournalPrintISSN>0016-7835</JournalPrintISSN><JournalElectronicISSN>1432-1149</JournalElectronicISSN><JournalTitle>Geologische Rundschau</JournalTitle><JournalAbbreviatedTitle>Geol Rundsch</JournalAbbreviatedTitle><JournalSubjectGroup><JournalSubject Type="Primary">Geosciences</JournalSubject><JournalSubject Type="Secondary">Geology</JournalSubject><JournalSubject Type="Secondary">Geophysics/Geodesy</JournalSubject></JournalSubjectGroup></JournalInfo><Volume><VolumeInfo VolumeType="Regular" TocLevels="0"><VolumeIDStart>63</VolumeIDStart><VolumeIDEnd>63</VolumeIDEnd><VolumeIssueCount>3</VolumeIssueCount></VolumeInfo><Issue IssueType="Regular"><IssueInfo TocLevels="0"><IssueIDStart>2</IssueIDStart><IssueIDEnd>2</IssueIDEnd><IssueArticleCount>24</IssueArticleCount><IssueHistory><CoverDate><Year>1974</Year><Month>7</Month></CoverDate></IssueHistory><IssueCopyright><CopyrightHolderName>Ferdinand Enke Verlag Stuttgart</CopyrightHolderName><CopyrightYear>1974</CopyrightYear></IssueCopyright></IssueInfo><Article ID="Art4"><ArticleInfo Language="En" ArticleType="OriginalPaper" NumberingStyle="Unnumbered" TocLevels="0" ContainsESM="No"><ArticleID>BF01820824</ArticleID><ArticleDOI>10.1007/BF01820824</ArticleDOI><ArticleSequenceNumber>4</ArticleSequenceNumber><ArticleTitle Language="En">Palaeomagnetic investigations of the tertiary and quaternary igneous rocks: VIII a palaeomagnetic and petrologic study of volcanics of the valley of Mexico</ArticleTitle><ArticleCategory>Aufsätze</ArticleCategory><ArticleFirstPage>451</ArticleFirstPage><ArticleLastPage>483</ArticleLastPage><ArticleHistory><RegistrationDate><Year>2005</Year><Month>5</Month><Day>18</Day></RegistrationDate></ArticleHistory><ArticleCopyright><CopyrightHolderName>Ferdinand Enke Verlag Stuttgart</CopyrightHolderName><CopyrightYear>1974</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>531</JournalID><VolumeIDStart>63</VolumeIDStart><VolumeIDEnd>63</VolumeIDEnd><IssueIDStart>2</IssueIDStart><IssueIDEnd>2</IssueIDEnd></ArticleContext></ArticleInfo><ArticleHeader><AuthorGroup><Author AffiliationIDS="Aff1" PresentAffiliationID="Aff1"><AuthorName DisplayOrder="Western"><Prefix>Prof. Ing.</Prefix><GivenName>Freddie</GivenName><FamilyName>Mooser</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff2" PresentAffiliationID="Aff2"><AuthorName DisplayOrder="Western"><Prefix>Prof. Dr.</Prefix><GivenName>Alan</GivenName><GivenName>E.</GivenName><GivenName>M.</GivenName><FamilyName>Nairn</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff3" PresentAffiliationID="Aff3"><AuthorName DisplayOrder="Western"><Prefix>Dr.</Prefix><GivenName>Jörg</GivenName><GivenName>F.</GivenName><GivenName>W.</GivenName><FamilyName>Negendank</FamilyName></AuthorName></Author><Affiliation ID="Aff1"><OrgDivision>Instituto de Geofisica</OrgDivision><OrgName>Universidad Nacional Autonoina</OrgName><OrgAddress><Street>Torre de Ciencias, Ciudad Universitaria</Street><Postcode>Mexico 20 D. F.</Postcode><City>Mexico</City></OrgAddress></Affiliation><Affiliation ID="Aff2"><OrgDivision>Department of Geology</OrgDivision><OrgName>University of South Carolina</OrgName><OrgAddress><Postcode>29208</Postcode><City>Columbia</City><State>S.C.</State><Country>USA</Country></OrgAddress></Affiliation><Affiliation ID="Aff3"><OrgName>Abt. Geowissenschaftliches Laboratorium der Fachgruppe Geographie der Universität Trier-Kaiserslautern</OrgName><OrgAddress><Street>D-55 Trier</Street><City>Schneidershof</City><Country>W-Germany</Country></OrgAddress></Affiliation></AuthorGroup><Abstract ID="Abs1" Language="De"><Heading>Zusammenfassung</Heading><Para>Das Becken von Mexiko befindet sich im Zentrum des Transmexikanischen Vulkangürtels, einer Ost-West-Struktur, die den nordamerikanischen Kontinent entlang des 19. Breitengrades durchschneidet.</Para><Para>Paläomagnetische Messungen legen die Vermutung nahe, daß 2 (Guadalupe- und Chichinautzin-Gruppe) der 7 vulkanischen Phasen, die das Becken formten, von wahrscheinlich kurzer Dauer waren. Die Chichinautzin-Gruppe, die das Becken im Süden abschnürte, muß sich grundsätzlich in den letzten 700 000 Jahren gebildet haben.</Para><Para>Die vulkanische Tätigkeit, die im Oligozän begann und sich kontinuierlich bis in dic heutige Zeit fortsetzte, förderte nachweislich im wesentlichen andesitische Produkte.</Para></Abstract><Abstract ID="Abs2" Language="En"><Heading>Abstract</Heading><Para>The basin of Mexico lies in the center of the Trans-Mexican Volcanic Belt, an east-west structure which dissects the North American Continent along the 19th parallel. Paleomagnetic measurements suggest that two of the seven eruptive phases —Guadalupe Group and Chichinautzin Group — that formed the basin, probably were of short duration; the Chichinautzin Group, which finally closed the basin to the south, must have been formed principally in the last 700,000 years.</Para><Para>The volcanic activity which began in Oligocene time and has continued until the present, has been proved to be essentially andesitic in composition.</Para></Abstract><Abstract ID="Abs3" Language="Fr"><Heading>Résumé</Heading><Para>Le bassin de Mexico se trouve au centre de la ceinture volcanique de Mexico, une structure est-ouest qui recoupe le continent nord-Americain près du 19<Superscript>e</Superscript> parallèle. Les mesures paléomagnétiques conduisent à supposer que deux des sept phases d'activités volcaniques, celles de la Guadaloupe et du Chichinautzin, étaient courtes. Les roches du Groupe de Chichinautzin, fermant le bassin au sud, ont été formées pendant les derniers 700,000 ans.</Para><Para>L'activité volcanique, qui a débuté à l'Oligocène et se continue encore actuellement a une charactère essentiellement andésitique.</Para></Abstract><Abstract ID="Abs4" Language="--"><Heading>Краткое содержание</Heading><Para>Мексиканский бассей н находится в центре трансмексиканского вулканического пояса — некой структу ры, которая пересекае т северо-американский материк</Para><Para>вдоль 19-й параллели с во стока на запад. Палеомагнитные изме рения разрешают пола гать, что две из семи вулканически х фаз, именно группа Guadalupe и Chichinautzin, образовавших этот бассейн, повсей вероя тности, были очень непродолжттельными. Группа Chichinautzin, продукты которой сос тавляют границу басс ейна на юге, появилась в последние 700000 лет.</Para><Para>Вулканическая деяте льность, начавшаяся в олигоцене и продолжающаяся непрерывно по сегодн я, подняла главным обр азом андезиты.</Para></Abstract></ArticleHeader><NoBody></NoBody></Article></Issue></Volume></Journal></Publisher></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Palaeomagnetic investigations of the tertiary and quaternary igneous rocks: VIII a palaeomagnetic and petrologic study of volcanics of the valley of Mexico</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Palaeomagnetic investigations of the tertiary and quaternary igneous rocks: VIII a palaeomagnetic and petrologic study of volcanics of the valley of Mexico</title></titleInfo><name type="personal"><namePart type="termsOfAddress">Prof. Ing.</namePart><namePart type="given">Freddie</namePart><namePart type="family">Mooser</namePart><affiliation>Instituto de Geofisica, Universidad Nacional Autonoina, Torre de Ciencias, Ciudad Universitaria, Mexico 20 D. F., Mexico</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="termsOfAddress">Prof. Dr.</namePart><namePart type="given">Alan</namePart><namePart type="given">E.</namePart><namePart type="given">M.</namePart><namePart type="family">Nairn</namePart><affiliation>Department of Geology, University of South Carolina, 29208, Columbia, S.C., USA</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="termsOfAddress">Dr.</namePart><namePart type="given">Jörg</namePart><namePart type="given">F.</namePart><namePart type="given">W.</namePart><namePart type="family">Negendank</namePart><affiliation>Abt. Geowissenschaftliches Laboratorium der Fachgruppe Geographie der Universität Trier-Kaiserslautern, D-55 Trier, Schneidershof, W-Germany</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="OriginalPaper"></genre><originInfo><publisher>Springer-Verlag</publisher><place><placeTerm type="text">Berlin/Heidelberg</placeTerm></place><dateIssued encoding="w3cdtf">1974-07-01</dateIssued><copyrightDate encoding="w3cdtf">1974</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="de">Zusammenfassung: Das Becken von Mexiko befindet sich im Zentrum des Transmexikanischen Vulkangürtels, einer Ost-West-Struktur, die den nordamerikanischen Kontinent entlang des 19. Breitengrades durchschneidet. Paläomagnetische Messungen legen die Vermutung nahe, daß 2 (Guadalupe- und Chichinautzin-Gruppe) der 7 vulkanischen Phasen, die das Becken formten, von wahrscheinlich kurzer Dauer waren. Die Chichinautzin-Gruppe, die das Becken im Süden abschnürte, muß sich grundsätzlich in den letzten 700 000 Jahren gebildet haben. Die vulkanische Tätigkeit, die im Oligozän begann und sich kontinuierlich bis in dic heutige Zeit fortsetzte, förderte nachweislich im wesentlichen andesitische Produkte.</abstract><abstract lang="en">Abstract: The basin of Mexico lies in the center of the Trans-Mexican Volcanic Belt, an east-west structure which dissects the North American Continent along the 19th parallel. Paleomagnetic measurements suggest that two of the seven eruptive phases —Guadalupe Group and Chichinautzin Group — that formed the basin, probably were of short duration; the Chichinautzin Group, which finally closed the basin to the south, must have been formed principally in the last 700,000 years. The volcanic activity which began in Oligocene time and has continued until the present, has been proved to be essentially andesitic in composition.</abstract><abstract lang="fr">Résumé: Le bassin de Mexico se trouve au centre de la ceinture volcanique de Mexico, une structure est-ouest qui recoupe le continent nord-Americain près du 19e parallèle. Les mesures paléomagnétiques conduisent à supposer que deux des sept phases d'activités volcaniques, celles de la Guadaloupe et du Chichinautzin, étaient courtes. Les roches du Groupe de Chichinautzin, fermant le bassin au sud, ont été formées pendant les derniers 700,000 ans. L'activité volcanique, qui a débuté à l'Oligocène et se continue encore actuellement a une charactère essentiellement andésitique.</abstract><abstract lang="--">Краткое содержание: Мексиканский бассей н находится в центре трансмексиканского вулканического пояса — некой структу ры, которая пересекае т северо-американский материк вдоль 19-й параллели с во стока на запад. Палеомагнитные изме рения разрешают пола гать, что две из семи вулканически х фаз, именно группа Guadalupe и Chichinautzin, образовавших этот бассейн, повсей вероя тности, были очень непродолжттельными. Группа Chichinautzin, продукты которой сос тавляют границу басс ейна на юге, появилась в последние 700000 лет. Вулканическая деяте льность, начавшаяся в олигоцене и продолжающаяся непрерывно по сегодн я, подняла главным обр азом андезиты.</abstract><note>Aufsätze</note><relatedItem type="host"><titleInfo><title>Geologische Rundschau</title></titleInfo><titleInfo type="abbreviated"><title>Geol Rundsch</title></titleInfo><genre type="journal" displayLabel="Archive Journal"></genre><originInfo><dateIssued encoding="w3cdtf">1974-07-01</dateIssued><copyrightDate encoding="w3cdtf">1974</copyrightDate></originInfo><subject><genre>Geosciences</genre><topic>Geology</topic><topic>Geophysics/Geodesy</topic></subject><identifier type="ISSN">0016-7835</identifier><identifier type="eISSN">1432-1149</identifier><identifier type="JournalID">531</identifier><identifier type="IssueArticleCount">24</identifier><identifier type="VolumeIssueCount">3</identifier><part><date>1974</date><detail type="volume"><number>63</number><caption>vol.</caption></detail><detail type="issue"><number>2</number><caption>no.</caption></detail><extent unit="pages"><start>451</start><end>483</end></extent></part><recordInfo><recordOrigin>Ferdinand Enke Verlag Stuttgart, 1974</recordOrigin></recordInfo></relatedItem><identifier type="istex">3EEA6FC2E3A41D97072D6C2366A74497AE27EA84</identifier><identifier type="DOI">10.1007/BF01820824</identifier><identifier type="ArticleID">BF01820824</identifier><identifier type="ArticleID">Art4</identifier><accessCondition type="use and reproduction" contentType="copyright">Ferdinand Enke Verlag Stuttgart, 1974</accessCondition><recordInfo><recordContentSource>SPRINGER</recordContentSource><recordOrigin>Ferdinand Enke Verlag Stuttgart, 1974</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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