Der Ostteil des Transmexikanischen Vulkangürtels und seine Position im Gesamtgürtel
Identifieur interne : 000766 ( Istex/Curation ); précédent : 000765; suivant : 000767Der Ostteil des Transmexikanischen Vulkangürtels und seine Position im Gesamtgürtel
Auteurs : J. F. W. Negendank ; H. Böhnel ; R. Emmermann [Allemagne] ; R. Krawczyk [Allemagne] ; 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
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J. F. W. Negendank<affiliation><mods:affiliation>Geologie der Fachgruppe Geographie/Geowissenschaften der Universität, D-5500, Trier</mods:affiliation>
<wicri:noCountry code="subField">Trier</wicri:noCountry>
</affiliation>
<affiliation><mods:affiliation>Institut für Geophysik der Universität, D-4400, Münster</mods:affiliation>
<wicri:noCountry code="subField">Münster</wicri:noCountry>
</affiliation>
<affiliation><mods:affiliation>Comision Federal de Electricidad, Mexico-City, Mexico 10.D.F.</mods:affiliation>
<wicri:noCountry code="subField">10.D.F.</wicri:noCountry>
</affiliation>
<affiliation><mods:affiliation>Comision Federal de Electricidad, Mexico-City, Mexico 10.D.F.</mods:affiliation>
<wicri:noCountry code="subField">10.D.F.</wicri:noCountry>
</affiliation>
<affiliation><mods:affiliation>Institut für Geowissenschaften der Universität, Lehreinheit Mineralogie, D-6500, Mainz</mods:affiliation>
<wicri:noCountry code="subField">Mainz</wicri:noCountry>
</affiliation>
Le document en format XML
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<front><div type="abstract" xml: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.</div>
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