Abstract
U–Pb geochronology of Variscan granitoid rocks from the West Asturian Leonese Zone of the NW Iberian belt documents the episodic nature of magmatism in this section of the western European Variscides. Each magmatic episode is characterized by granitoids with distinct features and has a duration on the scale of several millions of years. The ages of these granitoids place new constraints on the age and duration of magmatic and tectonic events, that are consistent with previous structural studies and proposed models for the tectonic evolution and migration of deformation in the NW Iberian Variscan belt. Granitoid rocks in this zone belong to two main magmatic episodes (syn‐ and post‐tectonic relative to the Variscan Orogeny) and are broadly representative of the granitoid types found in the NW Iberian Variscan belt. The syntectonic association is formed by: (i) tonalite–granodiorite–monzogranite intrusions emplaced synchronously with the main phase of crustal deformation (D 2 ) at c. 325 Ma and (ii) younger leucogranite intrusions emplaced synchronously with syn‐convergence extensional structures at c. 320–310 Ma. The post‐tectonic association is composed of: (i) volumetrically dominant tonalite–granodiorite–monzogranite intrusions (and associated minor mafic‐intermediate rocks) emplaced at c. 295–290 Ma; and (ii) scarce leucogranite intrusions emplaced at c. 290–285 Ma.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.