1887

Abstract

Sedimentological analysis and biostratigraphic review of the Oligo-Miocene deposits of northern Tunisia provide new data allowing new stratigraphic and paleogeographic reconstruction. The Kroumirie and Zouza member have the same age and correspond to sand/mud and mud/sand rich systems of a deep sea fan system with a detrital influx supplied from the North. Structural analysis demonstrate that the Numidian flysch has been displaced by a major thrust fault.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.20146481
2007-02-26
2020-07-13
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20146481
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