Tectonic escape of a crustal fragment during the closure of the Rheic Ocean: U–Pb detrital zircon data from the Late Palaeozoic Pulo do Lobo and South Portuguese zones, southern Iberia-Reference-Cited by-同舟云学术

Tectonic escape of a crustal fragment during the closure of the Rheic Ocean: U–Pb detrital zircon data from the Late Palaeozoic Pulo do Lobo and South Portuguese zones, southern Iberia

Published:2011-02-24 Issue:2 Volume:168 Page:383-392
ISSN:0016-7649
Container-title:Journal of the Geological Society
language:en
Short-container-title:Journal of the Geological Society

Author:

Braid James A.,Murphy J. Brendan,Quesada Cecilio,Mortensen Jim

Publisher

Geological Society of London

Subject

Geology

Reference83 articles.

1. Rheic Ocean ophiolitic remnants in southern Iberia questioned by SHRIMP U-Pb zircon ages on the Beja-Acebuches amphibolites

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3. Conodont faunas from Portugal and southwestern Spain. Part 6: A Lower Famenian conodont fauna at Monte do Formo da Cal (South Portugal);Boogaard;Scripta Geol,1981

4. Structural analysis of an accretionary prism in a continental collisional setting, the Late Paleozoic Pulo do Lobo Zone, Southern Iberia

5. Significance of MORB-derived Amphibolites from the Aracena Metamorphic Belt, Southwest Spain

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