Differentiate allogenic and autogenic controls on the formation of parasequences and depositional sequences of a tide‐ and wave‐dominated carbonate platform (Lower Cretaceous,Kopet‐DaghBasin, Iran)

Author:

Sharafi Mahmoud1,Reolid Matías2,Bayet‐Goll Aram3ORCID,Mohamadi Maryam4,Khanehbad Mohammad4,Mahboubi Asadollah4,Moussavi‐Harami Reza4

Affiliation:

1. Department of Geology, Faculty of Science University of Hormozgan Bandar Abbas Iran

2. Departamento de Geología Universidad de Jaén Jaén Spain

3. Department of Earth Sciences Institute for Advanced Studies in Basic Sciences (IASBS) Zanjan Iran

4. Department of Geology, Faculty of Science Ferdowsi University of Mashhad Mashhad Iran

Publisher

Wiley

Subject

Geology

Reference109 articles.

1. Biostratigraphy of the Tirgan Fm. in the Messino section, W Kopet‐Dagh;Abbasi F.;Geological Research,2013

2. Afshar‐Harb A.(1979).The stratigraphy tectonics and petroleum geology of the Kopet‐Dagh region northern Iran. (PhD thesis). Imperial College of Sciences and Technology University of London(p.316).

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