Structural Development of a Major Late Cenozoic Basin and Transpressional Belt in Central Iran: the Central Basin in the Qom-Saveh Area
Structural development of a major late Cenozoic basin and transpressional belt in central Iran: The Central Basin in the Qom-Saveh area Chris K. Morley PTTEP (PTT Exploration and Production), Offi ce Building, 555 Vibhavadi Rangsit Road, Chatuchak, Bangkok 10900, Thailand Booncherd Kongwung PTTEP (PTT Exploration and Production), Tehran Branch Offi ce, Unit 5 & 6, 5th Floor Sayeh Tower, Vali-e-Asr Avenue, 19677 13671 Tehran, Iran Ali A. Julapour Mohsen Abdolghafourian Mahmoud Hajian National Iranian Oil Company (NIOC) Exploration Directorate, 1st Dead-end, Seoul St., NE Sheikh Bahaei Sq., P.O. Box 19395-6669 Tehran, Iran Douglas Waples Consultant, PTTEP (PTT Exploration and Production), 555 Vibhavadi Rangsit Road, Chatuchak, Bangkok 10900, Thailand John Warren* Shell Chair in Carbonate Studies, Sultan Qaboos University, P.O. Box 17, Postal Code Al-Khodh-123, Muscat, Sultanate of Oman Heiko Otterdoom PTTEP (PTT Exploration and Production), Tehran Branch Offi ce, Unit 5 & 6, 5th Floor Sayeh Tower, Vali-e-Asr Avenue, 19677 13671 Tehran, Iran Kittipong Srisuriyon PTTEP (PTT Exploration and Production), Offi ce Building, 555 Vibhavadi Rangsit Road, Chatuchak, Bangkok 10900, Thailand Hassan Kazemi PTTEP (PTT Exploration and Production), Tehran Branch Offi ce, Unit 5 & 6, 5th Floor Sayeh Tower, Vali-e-Asr Avenue, 19677 13671 Tehran, Iran ABSTRACT as 4–5 km of Upper Red Formation section of Upper Red Formation were deposited being deposited in some parts of the basin in the main depocenters. Northwest-south- The Central Basin of the Iran Plateau during this stage. The upper part of the east– to north-northwest–south-southeast– is between the geologically better-known Upper Red Formation is associated with a striking dextral strike-slip to compressional regions of the Zagros and Alborz Moun- change to transpressional deformation, with faults dominate the area, with subordinate tains.
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