Sedimentary facies, depositional environment, and sequence stratigraphy of Oligocene–Miocene shallow water carbonate from the Rig Mountain, Zagros basin (SW Iran)

Author:

Adabi Mohammad H.,Kakemem Umid,Sadeghi Abbas

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Reference64 articles.

1. Abreu VS, Haddad GA (1998) Glacioeustatic variations: the mechanism linking stable isotope events and sequence stratigraphy from the early Oligocene to Middle Miocene. SEPM Spec Publ 60:245–260

2. Adabi MH, Asadi Mehmandosti E (2008) Microfacies and geochemistry of the Ilam Formation in the Tang-E Rashid area, Izeh, S.W. Iran. J Asian Earth Sci 33:267–277. doi: 10.1016/j.jseaes.2008.01.002

3. Adams CG, Bourgeois E (1967) Asmari biostratigraphy. Geological and exploration division. IOOC Rep 1074 (unpublished)

4. Alavi M (2004) Regional stratigraphy of the Zagros fold-thrust belt of Iran and its proforeland evolution. Am J Sci 304:1–20. doi: 10.2475/ajs.304.1.1

5. Alavi M (2007) Structures of the Zagros Fold-thrust belt in Iran. Am J Sci 307:1064–1095. doi: 10.2475/09.2007.02

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