1887
PDF

Abstract

The Cenozoic strata of the Mesopotamian Basin contain important reservoirs and seals, and they recorded the basin-filling history of the Zagros Foreland Basin. The Neogene clastic interval has been considered as foredeep and wedge-top deposits. The tectono-stratigraphic setting of the Paleogene interval has received less attention. We have revised the Paleocene-Early Miocene stratigraphy in the central Mesopotamian Basin to provide constraints on the early evolution of the Zagros Foreland Basin.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609-pdb.287.1178675
2012-03-04
2024-04-26
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.287.1178675
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