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~ 610 Ma: a critical age for the Iberian consolidation

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Abstract(s)

ABSTRACT: Both the Pan-African orogenic cycle and the peri-Gondwanan Cadomian Orogeny took part in the global tectonic event that led to the rearrangement of Gondwana's west-northern block. An approach to determine the nature of Cadomian - Pan-African events using detrital zircons population from Neoproterozoic-Lower Paleozoic (rift-to-drift cycle) stratigraphic record in Iberian Massif is here discussed.

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AIMS OF THE MEETING: The scientific sessions will be focused on the Pan-African and Cadomian Orogenies recorded in North Africa and western Europe across the Ediacaran Cambrian transition and its bearing in the assembly and demise of Pannotia. Contributions dealing with structural, magmatic, provenance sources, palaeomagnetic, sedimentary, chronostratigraphic and radiometric constraints are particularly welcome. ORGANIZING COMMITTEE: J. Javier Álvaro, Instituto de Geociencias (CSIC-UCM), Spain Martim Chichorro, Universidade Nova de Lisboa, Portugal Gabriel Gutiérrez-Alonso, Universidad de Salamanca, Spain.

Keywords

Cadomian orogeny Gondwana Neoproterozoic Iberian Massif

Citation

Chichorro, M., Solá, A. R., Crispim, L. - ~ 610 Ma: a critical age for the Iberian consolidation. In: The Panafrican and Cadomian orogenies in North Africa and Western Europe. Eds. J. Javier Álvaro, Martim Chichorro, Gabriel Gutiérrez-Alonso. IGEO, 2021, p. 10.

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IGEO - Instituto de Geociencias

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