Abstract
The worldwide sea-level fluctuations during the Pyrenean Orogeny caused substantial regressions in the north of Central Iran during the Eocene-Oligocene time. These orogenic activities shaped shallow marginal marine basins in some regions, which were sites for subsequent evaporite deposition.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
