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RISDepositional environments and ichnology of the deep-marine succession of the Amiran Formation (upper Maastrichtian–Paleocene), Lurestan Province, Zagros Fold–Thrust Belt, Iran
-bedded, and coarse-grained turbidite succession.
Deep marine paleoenvironments from basin slope to basin floor settings are preserved. These strata contain a diverse and abundant pre- and post-depositional ichnofauna. Proximal and axial parts of the sandy...
Depositional environments and ichnology of Upper Cretaceous deep-marine deposits in the Sistan Suture Zone, Birjand, Eastern Iran
. The Sefidabeh basin of turbidite origin consists of 10 sedimentary facies,which can be grouped into 3 facies associations (FA) representing submarine channel-related facies
associations (FA1), lobe-related facies associations (FA2), distal fan-basin floor...
Jurassic deep-water fans in the Neo-Tethys Ocean: The Kashafrud Formation of the Kopet-Dagh Basin, Iran
transport to deeper water. Coarse sands, extrabasinal pebbles, and plant fragments are present throughout the formation, and a thick boulder conglomerate unit lies within the turbidite succession. These observations suggest proximity to terrestrial sources...