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Depositional environment of the Bagh-e-Vang Formation – the only occurrence of upper Lower Permian in Iran

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EN
Abstrakty
EN
A transgression of the Tethys Ocean occurred in east central Iran, like in other areas of the Tethys Ocean, around the Yakhtashian/Bolorian (regional chronostratigraphical units corresponding with the Artinskian/Kungurian of the Early Permian) transition. This led to the development of a carbonate platform that is represented in the Shirgesht area on the northern part of the Tabas Block by the Bagh-e-Vang Formation, which constitutes the only known sedimentary unit from the late Early Permian in Iran. Field data and thin-section analysis indicate deposition on a carbonate ramp with barriers separating a lagoonal area with intertidal mud flats from the open-marine environment. The overall transgres-sive development is indicated by the presence of open-marine sediments on top of the barrier and lagoonal sediments.
Czasopismo
Rocznik
Strony
1--14
Opis fizyczny
Bibliogr. 50 poz.
Twórcy
  • Geology Department, Faculty of Sciences, Lorestan University, Lorestan, Iran
  • College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao 266590, China
  • Geology Department, Faculty of Sciences, Lorestan University, Lorestan, Iran
  • Geology Department, Faculty of Sciences, Lorestan University, Lorestan, Iran
  • Geology Department, Faculty of Sciences, Lorestan University, Lorestan, Iran
Bibliografia
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Uwagi
Opracowanie rekordu ze środków MNiSW, umowa Nr 461252 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2021).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-fea67e19-b7dc-4a82-a102-a34ff473a2f0
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