Ediacaran–Palaeozoic tectonic evolution of the Ossa Morena and Central Iberian zones (SW Iberia) as revealed by Sm–Nd isotope systematics

@article{LpezGuijarro2008EdiacaranPalaeozoicTE,
  title={Ediacaran–Palaeozoic tectonic evolution of the Ossa Morena and Central Iberian zones (SW Iberia) as revealed by Sm–Nd isotope systematics},
  author={Rafael L{\'o}pez-Guijarro and Maider Armend{\'a}riz and Cecilio Quesada and Javier Fern{\'a}ndez-Su{\'a}rez and J. Brendan Murphy and Christian Pin and F. Bellido},
  journal={Tectonophysics},
  year={2008},
  volume={461},
  pages={202-214}
}

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References

SHOWING 1-10 OF 203 REFERENCES
Geochronological constraints on the evolution of a suture: the Ossa-Morena/Central Iberian contact (Variscan Belt, south-west Iberian Peninsula)
One of the main tectonic boundaries of the Variscan Belt in the Iberian Peninsula is the Ossa-Morena/Central Iberian contact. This contact is marked by a highly deformed unit (Central Unit) which
The northern Ossa-Morena Cadomian batholith (Iberian Massif): magmatic arc origin and early evolution
Diorites and related rocks in the Mérida area of northern Ossa-Morena (SW Iberia) are intrusive into Precambrian metavolcanic and metasedimentary sequences. Cumulate products from the H2O-rich magmas
Neoproterozoic-early Palaeozoic tectonostratigraphy and palaeogeography of the peri-Gondwanan terranes: Amazonian v. West African connections
Abstract Within the Appalachian–Variscan orogen of North America and southern Europe lie a collection of terranes that were distributed along the northern margin of West Gondwana in the late
...
...