Cadomian metabasites of the eastern pyrenees revisited

HIGHLIGHTS

• who: Pan-African. Cadomian. Inherited zircon. et al. from the Departamento Ciencias Tierra y del Medio AmbienteFacultad Ciencias, Universidad Alicante have published the research: Cadomian metabasites of the Eastern Pyrenees revisited, in the Journal: (JOURNAL)

SUMMARY

The Pyrenees is an E-W trending Alpine belt formed between the Late Cretaceous and the Miocene by the convergence between the Iberian and European plates (Muñoz, 1992). Due to the tectonic stacking of several Alpine thrust-sheets, pre-Variscan basement rocks form a large strip in the core of the cordillera and provide evidence of . . .

 



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