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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.

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/content/papers/10.3997/2214-4609-pdb.287.1178675
2012-03-04
2021-10-19
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.287.1178675
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