Asadollah Mahboubi

TL;DR: In this article, historical documents and geological records have been combined to reconstruct Caspian sea-level (CSL) changes during the last millennium, and the overall results indicate a highstand during the Little Ice Age, up to −21 m (and extra rises due to manmade river avulsion), with a −28 m low-stand during Medieval Climate Anomaly, while presently the CSL stands at −26.5 m.

TL;DR: A variety of ribbon carbonates of the Deh-Sufiyan Formation (Middle Cambrian) in Central Alborz Range of northern Iran are studied to provide facies characterization and paleoenvironmental interpretation as mentioned in this paper.

TL;DR: Based on their lithologic characteristics and stratal geometries, the Middle Cambrian Fasham and Deh-Sufiyan Formations in the Central Alborz, northern Iran, exhibit 39 lithofacies representing several supratidal to deep subtidal facies belts.

TL;DR: In this article, the authors used petrophysical and geological data, by means of the neural network clustering technique, to identify rock types in the Oligo-Miocene Asmari Formation, which extends over the entire Zagros foreland basin.

TL;DR: In this article, the authors proposed a revision of the upper Lower Cambrian (Series 2-Series 3 boundary interval) through lowermost Ordovician lithostratigraphy of northern and central Iran.