The elusive nature of the Rheic Ocean suture in SW Iberia

The Rheic Ocean suture resulted from pre‐Carboniferous oceanic subduction followed by Late Devonian‐Carboniferous Variscan collision. In SW Iberia, this suture has been classically located along the boundary between the Ossa‐Morena and South Portuguese Zones based on the presence of three units: (i)...

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Veröffentlicht in:	Tectonics (Washington, D.C.) D.C.), 2015-12, Vol.34 (12), p.2429-2450
Hauptverfasser:	Pérez-Cáceres, I., Martínez Poyatos, D., Simancas, J. F., Azor, A.
Format:	Artikel
Sprache:	eng
Schlagworte:	Basalt Basins Beja-Acebuches Unit Carboniferous Devonian Geological time Iberian Variscides Left-lateral oblique collision Peramora Mélange Plate tectonics Pulo do Lobo unit Seismology
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