Post-Variscan evolution of the Anti-Atlas belt of Morocco constrained from low-temperature geochronology-Reference-Cited by-同舟云学术

Post-Variscan evolution of the Anti-Atlas belt of Morocco constrained from low-temperature geochronology

Published:2016-04-20 Issue:2 Volume:106 Page:593-616
ISSN:1437-3254
Container-title:International Journal of Earth Sciences
language:en
Short-container-title:Int J Earth Sci (Geol Rundsch)

Author:

Gouiza M.,Charton R.,Bertotti G.,Andriessen P.,Storms J. E. A.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://link.springer.com/content/pdf/10.1007/s00531-016-1325-0.pdf

Reference117 articles.

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3. André JP (1986) Bioconstruction carbonatée et faciès associés du Koudiat Lahmara, Jebilet orientales (Maroc Hercynien): un épisode récifal au Viséen supérieur. Eclogae Geologicae Helvetica 79:1–25. doi: 10.5169/seals-165836

4. Baidder L, Raddi Y, Tahiri M, Michard A (2008) Devonian extension of the Pan-African crust north of the West African craton, and its bearing on the Variscan foreland deformation: evidence from eastern Anti-Atlas (Morocco). In: Geological Society, London, Special Publications, pp 453–465

5. Barbero L, Teixell A, Arboleya M et al (2007) Jurassic-to-present thermal history of the central High Atlas (Morocco) assessed by low-temperature thermochronology. Terra Nova 19:58–64. doi: 10.1111/j.1365-3121.2006.00715.x

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