Stratigraphic architecture and depositional–diagenetic evolution of Oligocene–Miocene carbonate–evaporite platform in the southern margin of the Neo-Tethys Ocean, Lurestan zone of Zagros, Iran

Author:

Mohammadi Zahra,Mehrabi Hamzeh,Gharechelou Sajjad,Jalali Mahmoud,Swennen Rudy

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference98 articles.

1. Neogene salt in SW Iran and its interaction with Zagros folding;Abdollahie Fard;Geol. Mag.,2011

2. Sedimentary facies, depositional environment, and sequence stratigraphy of Oligocene-Miocene shallow water carbonate from the Rig Mountain, Zagros basin (SW Iran);Adabi;Carbonates Evaporites,2016

3. Adams, T., Bourgeois, F. 1967. Asmari biostratigraphy. Iranian Oil Operating Companies (IOOC). Technical Report 1074. NIOCEXP Office Tehran (unpublished).

4. Geology of Carbonate Reservoirs;Ahr,2008

5. Structures of the Zagros fold-thrust belt in Iran;Alavi;Am. J. Sci.,2007

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