Rojo Pérez, EstherDruguet, ElenaCasas, Josep M.Proenza Fernández, Joaquin AntonioFuenlabrada Pérez, José ManuelSánchez Martínez, SoniaGarcia Casco, AntonioArenas Martín, Ricardo2023-11-072023-11-072023-100301-926810.1016/j.precamres.2023.107186https://hdl.handle.net/20.500.14352/88634The North African margin of Gondwana formed by subduction and accretion during Ediacaran to Cambrian times. Sections of this active margin were incorporated during the late Paleozoic to the Variscan and Appalachian orogens. In the Variscan realm, these sections define in some regions a Cadomian basement comprising thick metasedimentary series associated with coeval subduction-related magmatic rock dated in the range 650–500 Ma. In the Cap de Creus Massif (Eastern Pyrenean domain), the Cadomian metasedimentary rocks formed from sediments derived from mixed felsic and intermediate/mafic sources, intruded by granitoid and minor mafic igneous rocks. These series were formed in a peri-Gondwanan volcanic arc setting, like other Cadomian series described in the SW of the Iberian Massif, such as Serie Negra Group of the Ossa Morena Complex. However, the Nd model ages of the Cap de Creus metasedimentary samples range from 1431 to 1620 Ma and are younger than those of their SW Iberia equivalents. This result can be interpreted as an indication of an eastern location in the Ediacaran - Cambrian peri-Gondwanan magmatic arc. Furthermore, the Cadomian series in the Central Iberian Zone have even younger Nd model ages than those of SW and NE Iberia. We present two end-member paleogeographic models consistent with reconstruction of the initial location of the Cap de Creus Massif and its relations with other domains (Ossa Morena Complex and Central Iberian Zone) in this sector of the North African Gondwanan margin.engjournal article1872-7433https://doi.org/10.1016/j.precamres.2023.107186https://www.sciencedirect.com/science/article/pii/S0301926823002267restricted access552.4Gondwana marginArc-related seriesEdiacaran-Cambrian timeIsotopic sourcesPetrología2506.13 Petrología Ignea y Metamórfica