Der Ostteil des Transmexikanischen Vulkangürtels und seine Position im Gesamtgürtel
Identifieur interne : 000816 ( Istex/Corpus ); précédent : 000815; suivant : 000817Der Ostteil des Transmexikanischen Vulkangürtels und seine Position im Gesamtgürtel
Auteurs : J. F. W. Negendank ; H. Böhnel ; R. Emmermann ; R. Krawczyk ; F. Mooser ; S. Soto Pinieda ; H. J. TobschallSource :
- Naturwissenschaften [ 0028-1042 ] ; 1982-03-01.
Abstract
Abstract: It is reported about geological and petrological investigations on igneous rocks of the Eastern Trans-Mexican volcanic belt. The results seem to coincide with the hypothesis of the Cocosplate being subducted in NE direction.
Url:
DOI: 10.1007/BF00376717
Links to Exploration step
ISTEX:F7DA5CF6B07792D7941C530E5F483FC85DF3CEABLe document en format XML
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AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>J.</GivenName><GivenName>F.</GivenName><GivenName>W.</GivenName><FamilyName>Negendank</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff2"><AuthorName DisplayOrder="Western"><GivenName>H.</GivenName><FamilyName>Böhnel</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff3"><AuthorName DisplayOrder="Western"><GivenName>R.</GivenName><FamilyName>Emmermann</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff3"><AuthorName DisplayOrder="Western"><GivenName>R.</GivenName><FamilyName>Krawczyk</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff4"><AuthorName DisplayOrder="Western"><GivenName>F.</GivenName><FamilyName>Mooser</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff4"><AuthorName DisplayOrder="Western"><GivenName>S.</GivenName><FamilyName>Soto Pinieda</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff5"><AuthorName DisplayOrder="Western"><GivenName>H.</GivenName><GivenName>J.</GivenName><FamilyName>Tobschall</FamilyName></AuthorName></Author><Affiliation ID="Aff1"><OrgName>Geologie der Fachgruppe Geographie/Geowissenschaften der Universität</OrgName><OrgAddress><Postcode>D-5500</Postcode><City>Trier</City></OrgAddress></Affiliation><Affiliation ID="Aff2"><OrgName>Institut für Geophysik der Universität</OrgName><OrgAddress><Postcode>D-4400</Postcode><City>Münster</City></OrgAddress></Affiliation><Affiliation ID="Aff3"><OrgName>Institut für Petrographie und Geochemie der Universität</OrgName><OrgAddress><Postcode>D-7500</Postcode><City>Karlsruhe</City></OrgAddress></Affiliation><Affiliation ID="Aff4"><OrgName>Comision Federal de Electricidad</OrgName><OrgAddress><City>Mexico-City</City><Country>Mexico 10.D.F.</Country></OrgAddress></Affiliation><Affiliation ID="Aff5"><OrgDivision>Institut für Geowissenschaften der Universität</OrgDivision><OrgName>Lehreinheit Mineralogie</OrgName><OrgAddress><Postcode>D-6500</Postcode><City>Mainz</City></OrgAddress></Affiliation></AuthorGroup><Abstract ID="Abs1" Language="En"><Heading>Abstract</Heading><Para>It is reported about geological and petrological investigations on igneous rocks of the Eastern Trans-Mexican volcanic belt. The results seem to coincide with the hypothesis of the Cocosplate being subducted in NE direction.</Para></Abstract><ArticleNote Type="Misc"><SimplePara>Die Arbeiten wurden von der Deutschen Forschungsgemeinschaft (Ne 154/7/10) gefördert, wofür wir unseren Dank aussprechen.</SimplePara></ArticleNote></ArticleHeader><NoBody></NoBody></Article></Issue></Volume></Journal></Publisher></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="de"><title>Der Ostteil des Transmexikanischen Vulkangürtels und seine Position im Gesamtgürtel</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="de"><title>Der Ostteil des Transmexikanischen Vulkangürtels und seine Position im Gesamtgürtel</title></titleInfo><name type="personal"><namePart type="given">J.</namePart><namePart type="given">F.</namePart><namePart type="given">W.</namePart><namePart type="family">Negendank</namePart><affiliation>Geologie der Fachgruppe Geographie/Geowissenschaften der Universität, D-5500, Trier</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">H.</namePart><namePart type="family">Böhnel</namePart><affiliation>Institut für Geophysik der Universität, D-4400, Münster</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">R.</namePart><namePart type="family">Emmermann</namePart><affiliation>Institut für Petrographie und Geochemie der Universität, D-7500, Karlsruhe</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">R.</namePart><namePart type="family">Krawczyk</namePart><affiliation>Institut für Petrographie und Geochemie der Universität, D-7500, Karlsruhe</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">F.</namePart><namePart type="family">Mooser</namePart><affiliation>Comision Federal de Electricidad, Mexico-City, Mexico 10.D.F.</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">S.</namePart><namePart type="family">Soto Pinieda</namePart><affiliation>Comision Federal de Electricidad, Mexico-City, Mexico 10.D.F.</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">H.</namePart><namePart type="given">J.</namePart><namePart type="family">Tobschall</namePart><affiliation>Institut für Geowissenschaften der Universität, Lehreinheit Mineralogie, D-6500, Mainz</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><dateCreated encoding="w3cdtf">1981-04-13</dateCreated><dateIssued encoding="w3cdtf">1982-03-01</dateIssued><copyrightDate encoding="w3cdtf">1982</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">de</languageTerm><languageTerm type="code" authority="iso639-2b">ger</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType></physicalDescription><abstract lang="en">Abstract: It is reported about geological and petrological investigations on igneous rocks of the Eastern Trans-Mexican volcanic belt. The results seem to coincide with the hypothesis of the Cocosplate being subducted in NE direction.</abstract><relatedItem type="host"><titleInfo><title>Naturwissenschaften</title></titleInfo><titleInfo type="abbreviated"><title>Naturwissenschaften</title></titleInfo><genre type="journal" displayLabel="Archive Journal"></genre><originInfo><dateIssued encoding="w3cdtf">1982-03-01</dateIssued><copyrightDate encoding="w3cdtf">1982</copyrightDate></originInfo><subject><genre>Life Sciences</genre><topic>Life Sciences, general</topic><topic>Environment, general</topic></subject><identifier type="ISSN">0028-1042</identifier><identifier type="eISSN">1432-1904</identifier><identifier type="JournalID">114</identifier><identifier type="IssueArticleCount">17</identifier><identifier type="VolumeIssueCount">12</identifier><part><date>1982</date><detail type="volume"><number>69</number><caption>vol.</caption></detail><detail type="issue"><number>3</number><caption>no.</caption></detail><extent unit="pages"><start>130</start><end>139</end></extent></part><recordInfo><recordOrigin>Springer-Verlag, 1982</recordOrigin></recordInfo></relatedItem><identifier type="istex">F7DA5CF6B07792D7941C530E5F483FC85DF3CEAB</identifier><identifier type="DOI">10.1007/BF00376717</identifier><identifier type="ArticleID">BF00376717</identifier><identifier type="ArticleID">Art5</identifier><accessCondition type="use and reproduction" contentType="copyright">Springer-Verlag, 1982</accessCondition><recordInfo><recordContentSource>SPRINGER</recordContentSource><recordOrigin>Springer-Verlag, 1982</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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