1887

Abstract

The Middle Pliocene deposits of the Neogene are widely developed covering all of the offshore South Caspian Basin, such adjacent onshore areas as Kura depression, Wester Turkmenistan, Apsheron and Cheleken peninsulas, and southern portion of the Tersk-Caspian trough. In each of these areas, the Middle Pliocene formation has different lithological structure and mineralogical composition, due to the difference in tectonic intensity and orientation, depositional environments and sources of clastic sediments.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201408583
1998-06-08
2021-08-05
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201408583
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