One hundred and forty‐four published successions of shallow‐water carbonates, deposited
between the Palaeocene and the Miocene, from the Levant to the Himalayas, have been re …

The main aim of this study is to integrate the results of sedimentology, strontium isotope with
the results simultaneous inversion of 3D seismic data for rock characterization of Rupelian …

The Asmari Formation deposited in the Zagros foreland basin during the Oligocene-
Miocene. Four different measured sections were studied in this area in order to interpret the …

Abstract The Asmari Formation is one of the most important prolific reservoirs along both
sides of the Persian Gulf. The present study aims to characterize the fractured dolomite of …

The distributions of sediment grain types and microfacies in two outcrop sections in the
central part of the Zagros Fold and Thrust Belt, Iran, are used to interpret changes in salinity …

Abstract The Asmari Formation is a thick carbonate succession of the Oligo-Miocene in
Zagros Mountains (southwest Iran). In order to interpret the facies and depositional …

Abstract The Asmari Formation in the G oilfield on the Iran-Iraq border is a fractured-porous
multi-lithology mixed reservoir, for which fracture is an important factor affecting oil …

The Asmari reservoir properties in various hydrocarbon fields across the Dezful Embayment
(SW Iran) are modified by dolomitization. Petrographic and geochemical analyses of the …

Abstract The Miocene Pirabas Formation is of strategic importance for the hydrocarbon
industry since it represents the onshore portion of larger offshore basins of Northern Brazil …

Abstract The Tale-Zang Formation in Zagros Mountains (south-west Iran) is a Lower to
Middle Eocene carbonate sequence. Carbonate sequences of the Tale-Zang Formation …