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Der Ostteil des Transmexikanischen Vulkangürtels und seine Position im Gesamtgürtel

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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.

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Die Arbeiten wurden von der Deutschen Forschungsgemeinschaft (Ne 154/7/10) gefördert, wofür wir unseren Dank aussprechen.

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Negendank, J.F.W., Böhnel, H., Emmermann, R. et al. Der Ostteil des Transmexikanischen Vulkangürtels und seine Position im Gesamtgürtel. Naturwissenschaften 69, 130–139 (1982). https://doi.org/10.1007/BF00376717

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  • DOI: https://doi.org/10.1007/BF00376717

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