𝔖 Bobbio Scriptorium
✦   LIBER   ✦

Triassic stratigraphy and structural evolution of a rift basin: the Eç Çour basin, High atlas of Marrakech, Morocco

✍ Scribed by El Hassane El Arabi; Jean Ferrandini; Rachid Essamoud

Book ID
108460195
Publisher
Elsevier Science
Year
2003
Tongue
English
Weight
812 KB
Volume
36
Category
Article
ISSN
1464-343X

No coin nor oath required. For personal study only.

📜 SIMILAR VOLUMES

Structural style and evolution of a Late
Structural style and evolution of a Late Triassic rift basin in the Central High Atlas, Morocco: controls on sediment deposition
✍ Catherine Baudon; Ivan Fabuel-Perez; Jonathan Redfern 📂 Article 📅 2009 🏛 John Wiley and Sons 🌐 English ⚖ 905 KB

## Abstract Late Triassic continental sediments deposited in an active‐rift setting are exposed in the Oukaimeden‐Ourika Valley, located in the Central High Atlas Basin of Morocco. The Oukaimeden Sandstone Formation is dominated by ephemeral and perennial braided fluvial facies, and is an outcrop a

Geological evolution and structural styl
Geological evolution and structural style of the Palaeozoic Tafilalt sub-basin, eastern Anti-Atlas (Morocco, North Africa)
✍ E. A. Toto; F. Kaabouben; L. Zouhri; M. Belarbi; M. Benammi; M. Hafid; L. Boutib 📂 Article 📅 2007 🏛 John Wiley and Sons 🌐 English ⚖ 943 KB

## Abstract The Tafilalt is one of a number of generally unexplored sub‐basins in the eastern Anti‐Atlas of Morocco, all of which probably underwent a similar tectono‐stratigraphic evolution during the Palaeozoic Era. Analysis of over 1000 km of 2‐D seismic reflection profiles, with the interpretat

A survey of multi-stage diagenesis and d
A survey of multi-stage diagenesis and dolomitization of Jurassic limestones along a regional shelf-to-basin transect in the Ziz Valley, Central High Atlas Mountains, Morocco
✍ L.B. Railsback; E.C. Hood 📂 Article 📅 2001 🏛 Elsevier Science 🌐 English ⚖ 827 KB

Petrographic and geochemical data from ®ve localities in the Ziz Valley of Morocco indicate that Jurassic limestones have undergone early diagenesis that varied with location from shelf to basinal settings, burial diagenesis that was most pronounced in basinal settings, and late diagenesis caused by