Paleoenvironmental significance of the carbon isotope record across the Cenomanian–Turonian transition and the Oceanic Anoxic Event 2 (OAE2) in the southeastern Neotethys, Zagros, Iran

Author:

Bagherpour BorhanORCID,Nkemata Andy F.,Vaziri–Moghaddam Hossein,Blattmann Thomas M.ORCID,Mohtadi MahyarORCID

Funder

Shiraz University

Publisher

Elsevier BV

Subject

Paleontology

Reference134 articles.

1. La geochimie isotopique du carbone (δ13 C) comme outil stratigraphique. Application a la limite Cenomanien/Turonien en Tunisie centrale;Accarie;Comptes Rendus de l'Academie des Sciences – Series IIA: Earth and Planetary Science,1996

2. Regional stratigraphy of the Zagros fold–thrust belt of Iran and its proforeland evolution;Alavi;American Journal of Science,2004

3. Structures of the Zagros fold–thrust belt in Iran;Alavi;American Journal of Science,2007

4. Sedimentary Basins and Petroleum Geology of the Middle East;Alsharhan,1997

5. A review of the Cretaceous formations in the Arabian Peninsula and the Gulf: Part II. Mid–Cretaceous (Wasia Group) stratigraphy and paleogeography;Alsharhan;Journal of Petroleum Geology,1988

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