1887

Abstract

Paleogene sedimentary basins which are characteristic for the Internides of the Western Carpathians were formed in the period from Senonian to Oligocene, i.e. after overthrusting of superficial Mesozoic nappes.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201409117
1996-06-04
2020-07-16
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409117
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