Depositional environment and sequence stratigraphy of the Oligo-Miocene Asmari Formation in SW Iran

H Vaziri-Moghaddam, M Kimiagari, A Taheri - Facies, 2006 - Springer
Abstract The Asmari Formation, a thick carbonate succession of the Oligo-Miocene in Zagros
Mountains (southwest Iran), has been studied to determine its microfacies …

Carbonate platform evolution of the Asmari Formation in the east of Dezful Embayment, Zagros Basin, SW Iran

A Khalili, H Vaziri-Moghaddam, M Arian… - Journal of African Earth …, 2021 - Elsevier
In this study, based on a multidisciplinary approach (biostratigraphy, cyclostratigraphy, and
facies analysis), the Asmari carbonate successions were evaluated across two platform-to …

[HTML][HTML] Oligocene-Miocene ramp system (Asmari Formation) in the NW of the Zagros basin, Iran: Microfacies, paleoenvironment and depositional sequence

H Vaziri-Moghaddam, A Seyrafian, A Taheri… - Revista mexicana de …, 2010 - scielo.org.mx
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 …

Facies analysis and palaeoenvironmental interpretation of the late Oligocene Attard Member (lower Coralline Limestone Formation), Malta

M Brandano, V Frezza, L Tomassetti, M Pedley… - …, 2009 - Wiley Online Library
The Oligocene represents a key interval during which coralline algae became dominant on
carbonate ramps and luxuriant coral reefs emerged on a global scale. So far, few studies …

Sedimentary facies and sequence stratigraphy of the Asmari Formation at chaman-Bolbol, Zagros Basin, Iran

M Amirshahkarami, H Vaziri-Moghaddam… - Journal of Asian Earth …, 2007 - Elsevier
The Oligocene–Miocene Asmari Formation of the Zagros Basin is a thick sequence of
shallow water carbonate. In the study area, it is subdivided into 14 microfacies that are …

Stratigraphic architecture and depositional–diagenetic evolution of Oligocene–Miocene carbonate–evaporite platform in the southern margin of the Neo-Tethys Ocean …

Z Mohammadi, H Mehrabi, S Gharechelou… - Journal of Asian Earth …, 2022 - Elsevier
Abstract The Oligocene–Miocene (OM) depositional sequences (Asmari Formation) are
marked by remarkable changes in thickness, lithology, depositional facies characteristics …

Microfacies and sedimentary environment of the Oligocene sequence (Asmari Formation) in Fars sub-basin, Zagros Mountains, southwest Iran

R Sadeghi, H Vaziri-Moghaddam, A Taheri - Facies, 2011 - Springer
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 …

Carbonate sediment dynamics in the Abu Dhabi lagoon-implications for low-angle inner-to-middle ramp models

Y Zhong, SW Lokier, CL Pederson, F Fiorini… - Marine Geology, 2023 - Elsevier
Carbonate ramps are prominent features of continental margins and intrashelf basins
throughout much of Earth's history. Among the limited number of recent analogues of ancient …

Sedimentary facies, depositional environment, and sequence stratigraphy of Oligocene–Miocene shallow water carbonate from the Rig Mountain, Zagros basin (SW …

MH Adabi, U Kakemem, A Sadeghi - Carbonates and evaporites, 2016 - Springer
This study investigates the depositional environment and sequence stratigraphy of the
Asmari Formation that is exposed at the Rig anticline in the Izeh zone of the Zagros foreland …

Oligo-Miocene carbonate platform evolution in the northern margin of the Asmari intra-shelf basin, SW Iran

MA Dill, H Vaziri-Moghaddam, A Seyrafian… - Marine and petroleum …, 2018 - Elsevier
This study is based on seven outcrops along a regional transect in the central subdivision of
the Zagros Foreland Basin. This NE-SW trending transect extends for 140 km and covers the …