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Arnaud Vanneau, A., Conard, M., Deloffre, R., et al. (1991) Distribution of Lower Cretaseous Foraminifera and Dasy-cladal Algae of the Adriatic Plate. In: Vlahovic, I. and Velic, I., Eds., Some Aspects of the Shallow Water Sedimentation on the Adriatic Carbonate Platform (Permian to Eocene), Inst. of Geology Zagreb, 22-26.

has been cited by the following article:

• TITLE: Benthic Foraminiferal and Calcareous Algae Assemblages in the Tirgan Formation (Urgonien Facies Type) in South Flank of Ghorogh Syncline (North of Chenaran), NE Iran

  AUTHORS: Hoda Yavarmanesh, Seyed Hamid Vaziri, Ali Asghar Aryaei, Davood Jahani, Mohsen Pourkermani, Ebrahim Khademi Bouriabadi

  KEYWORDS: Tirgan Formation, Ghorogh Syncline, Foraminifera, Calcareous Algae

  JOURNAL NAME: Open Journal of Geology, Vol.7 No.6, June 8, 2017

  ABSTRACT: In this research, the Tirgan Formation in the south flank of Ghorogh Syncline (north of Chenaran), northeastern Iran with the thickness of 251 was studied. This section consists of limestone, marly limestone and shale with impressions of echinoderms toxasteridae family, many of foraminifera from orbitolinidae family and also lots of calcareous algae that create facies variation along with other non-skeletal allochems. Micropaleontological investigation has been carried out on 90 thin-sections. These criteria reveal that an equivalent of the Urgonian facies type (in France-Swiss area) and open marine, low depth sedimentary basin are extended in the Kopet-Dagh basin. In this article, we tried to introduce some of the important foraminiferal and calcareous algal assemblages of this area.