Abstract :
[en] New interpretations of depositional palaeoenvironments in the Mississippian (Lower Carboniferous) Mobarak Formation (Alborz Mountains, Iran) suggest a significant and persistent influence of storms. This deviates from previous conclusions that these deposits recorded mounds, patch reefs, and extensive lagoons deposited under stagnant environmental conditions. We here clarify and discuss the origin and nature of this misconception by explaining “unexpected” observations that are informed by outdated interpretations of the depositional environment of the Mobarak Formation. This evaluation offers the context required for appropriately interpreting and correlating Mississippian depositional records across the Alborz Basin.
Sardar Abadi, Mehrdad; Rock Physics and Borehole Geophysics, LIAG, Leibniz Institute for Applied Geophysics, Hannover, Germany
Voeten, Dennis F. A. E.; Department of Organismal Biology, Subdepartment of Evolution and Development, Uppsala University, Uppsala, Sweden ; Museum of Evolution, Uppsala University, Uppsala, Sweden
Kulagina, Elena I.; Ufa Federal Research Center of the Russian Academy of Sciences, Institute of Geology, Ufa, Russian Federation
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