1887

Abstract

Sediments of Upper Oligocene age (Repel and Chatt) were deposited in a pull apart basin that was opened along the left lateral Inntal fault. Tectonic evidence for structuren of basin opening is poor. Adjacent to major normal faults it is possible to define the direction of opening of the basin by microtectonic methods. Additional information is given by facies pattems of the basin fill.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201410226
1994-06-10
2020-07-14
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410226
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