Supplementary material for "U-Pb geochronology of detrital and igneous zircon grains from the Águilas Arc in the Internal Betics (SE Spain): implications for Carboniferous-Permian paleogeography of Pangea"

Published: 3 November 2020| Version 1 | DOI: 10.17632/b2yrffk67s.1
Contributors:
ANTONIO JABALOY,
Cristina Talavera,
Martín J. Rodríguez-Peces,
Mercedes Vázquez-Vílchez,
Noreen J. Evans

Description

The Águilas Arc in SE Spain comprises the three tectonic complexes of the Internal Betic Chain, covered by unconformable Middle Miocene to recent sediments. New U-Pb detrital zircon data provide maximum protolith depositional ages, while zircon U-Pb zircon ages of metaigneous rocks yield further depositional age constraints.

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Institutions

Curtin University, Universidad de Granada, Edinburgh Napier University, Universidad Complutense de Madrid

Categories

Geology, Geochronology, Paleogeography, Uranium-Lead Dating, Zircon

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