1887

Abstract

A sequence stratigraphic model is proposed for the Oligo-Miocene Asmari and Pabdeh Formations in the Dezful Embayment of South-West Iran. The model is based on both detailed sedimentological observations in outcrops, core and well logs, and an improved high resolution chronostratigraphic framework constrained by Sr-isotope stratigraphy and biostratigraphy. The better understanding of the stratigraphic architecture allows distinguishing four, geographically separated types of Asmari reservoirs.

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/content/papers/10.3997/2214-4609.20145917
2009-05-04
2024-03-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20145917
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