The jbel saghro au (–ag, cu) and ag–hg metallogenetic province: Product of a long-lived ediacaran tectono-magmatic evolution in the moroccan anti-atlas
The Jbel Saghro is interpreted as part of a long-lived silicic large igneous province. The area
comprises two lithostructural complexes. The Lower Complex consists of folded …
comprises two lithostructural complexes. The Lower Complex consists of folded …
Cenozoic mountain building and topographic evolution in Western Europe: impact of billions of years of lithosphere evolution and plate kinematics
F Mouthereau, P Angrand… - BSGF-Earth …, 2021 - pubs.geoscienceworld.org
The architecture and tectono-magmatic evolution of the lithosphere of Europe are the result
of a succession of subduction, rifting and inputs from plumes that have modified the …
of a succession of subduction, rifting and inputs from plumes that have modified the …
Contribution to a geodynamic reconstruction of the Anti-Atlas (Morocco) during Pan-African times with the emphasis on inversion tectonics and metallogenic activity at …
D Gasquet, G Levresse, A Cheilletz… - Precambrian …, 2005 - Elsevier
New geochronological analyses (U–Pb SIMS zircon ages) have yielded ages of 552±5Ma
for the Bou Madine rhyolitic dome (Ougnat, eastern Anti-Atlas), 543±9Ma for the …
for the Bou Madine rhyolitic dome (Ougnat, eastern Anti-Atlas), 543±9Ma for the …
The boundaries of the West African craton, with special reference to the basement of the Moroccan metacratonic Anti-Atlas belt
N Ennih, JP Liégeois - Geological Society, London, Special …, 2008 - lyellcollection.org
Abstract The West African craton (WAC) was constructed during the Archaean and the c. 2
Ga Palaeoproterozoic Eburnian orogeny. Mesoproterozoic quiescence at c. 1.7–1.0 Ga …
Ga Palaeoproterozoic Eburnian orogeny. Mesoproterozoic quiescence at c. 1.7–1.0 Ga …
The variscan belt
A Michard, C Hœpffner, A Soulaimani… - Continental evolution: The …, 2008 - Springer
This chapter is a tribute to Jacques Destombes and Solange Willefert, and to the memory of
Henri Hollard, whose names are associated to the deciphering of the Paleozoic stratigraphy …
Henri Hollard, whose names are associated to the deciphering of the Paleozoic stratigraphy …
The moroccan hercynides
C Hoepffner, A Soulaimani, A Piqué - Journal of African Earth Sciences, 2005 - Elsevier
In Northern Africa deformed Paleozic rocks are observed, mainly in Morocco where they are
present in two structural domains:(i) the southern domain, ie the Anti-Atlas belt. In this …
present in two structural domains:(i) the southern domain, ie the Anti-Atlas belt. In this …
An expanded record of Early Cambrian carbon cycling from the Anti-Atlas Margin, Morocco
We present a δ 13C record from the Anti-Atlas mountains of Morocco and place it in the
context of a detailed regional tectonostratigraphy. We place the litho-and chemostratigraphic …
context of a detailed regional tectonostratigraphy. We place the litho-and chemostratigraphic …
Neoproterozoic tectonic evolution of the jebel Saghro and Bou Azzer—El Graara inliers, eastern and central Anti-Atlas, Morocco
GJ Walsh, F Benziane, JN Aleinikoff, RW Harrison… - Precambrian …, 2012 - Elsevier
New mapping, geochemistry, and 17 U–Pb SHRIMP zircon ages from rocks of the Sirwa,
Bou Azzer–El Graara, and Jebel Saghro inliers constrain the Neoproterozoic evolution of the …
Bou Azzer–El Graara, and Jebel Saghro inliers constrain the Neoproterozoic evolution of the …
[HTML][HTML] Tectonics of the anti-atlas of Morocco
M Burkhard, S Caritg, U Helg, C Robert-Charrue… - Comptes Rendus …, 2006 - Elsevier
The Anti-Atlas is reviewed and examined in the light of its geodynamic significance as a
Palaeozoic basin and fold belt. Shortening is accommodated by polyharmonic buckle …
Palaeozoic basin and fold belt. Shortening is accommodated by polyharmonic buckle …
Late Ediacaran–Cambrian structures and their reactivation during the Variscan and Alpine cycles in the Anti-Atlas (Morocco)
A Soulaimani, A Michard, H Ouanaimi, L Baidder… - Journal of African Earth …, 2014 - Elsevier
Abstract The post-Pan-African evolution of the northern border of the West African Craton is
largely controlled by the remobilisation of Late Neoproterozoic basement faults. The Upper …
largely controlled by the remobilisation of Late Neoproterozoic basement faults. The Upper …