1887

Abstract

B18 CONTRIBUTION OF ANALOGUE MODELING FOR THE UNDERSTANDING OF THE SAHARAN ATLAS STRUCTURE Abstract 1 The Saharan Atlas (Algeria) is an intracratonic mountain belt which developed at the southern margin of Tethys. It is 650 km long and varies in width from 90 to 140 km. Topographic elevations reach 2 000 m. It forms part of the Atlas orogenic system which occurs in North Africa from Morocco to Tunisia. During the Mesozoic up to 10 000 m of mixed continental and marine sediments were deposited unconformably above the Palaeozoic basement. This basement contains NE-SW and NW-SE Variscan fabrics and older

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609-pdb.11.B18
2005-04-10
2024-03-28
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.11.B18
Loading
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error