Late Paleocene to Early Eocene larger benthic foraminifera biozones and microfacies in Estahbanate area, Southwest of Iran with Thetyan biozones correlation

Author:

Amirshahkarami Mahnaz,Zebarjadi Elham

Funder

Payame Noor University

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Reference59 articles.

1. Adams TD, Bourgeois E (1967) Asmari biostratigraphy. IOOC, Report No 1074, pp 37 (Unpublished)

2. Aghaei A, Mahboubi A, Moussavi-Harami R, Nadjafi M (2010) Dolomite types of upper jurassic carbonate sediments based on petrography, SEM and EDS analysis—west of Bojnourd and Jajarm area. In: The Forth National geological conference. Payame Noor University, Mashad, Iran, pp 1682–1688

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

4. Allahkarampour Dill M, Seyrafian A, Vaziri-Moghaddam H (2010) The Asmari Formation, north of the Gachsaran (Dill anticline), southwest Iran: facies analysis, depositional environments and sequence stratigraphy. Carbonates Evaporites 25:145–160. https://doi.org/10.1007/s13146-010-0021-6

5. Amiri-Bakhtiar H, Norainejad Kh (2014) Stratigraphic review of the Zagros-Jahrum formation. Explor Prod J NIOC 1393(115):30–31 (In Persian)

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