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- W2181815500 abstract "The Lower Cretaceous limestones and marls in central part of Iran having recently been attended for hydrocarbon exploration by NIOC contain a comparatively rich assemblage of orbitolinids . The Barremian-Aptian orbitolinid bearing strata in this area are considered to constitute the Mesozoic main reservoir rocks in prospecting point of view. The detailed and satisfying stratigraphic results are of great importance for hydrocarbon exploration studies therefore this study tries to improve the knowledge of Lower Cretaceous shallow marine biostratigraphic studies in Central Iran using larger benthic foraminifera (mainly orbitolinids) constituting the main representatives of foraminiferal assemblage in this area. For the purpose of this study one section (Sarvestan) located in South of Esfahan was measured and sampled. Three assemblages of larger benthic foraminifera were recognized indicating Early Barremian to Late Aptian age (Eopalorbitolina assemblage = Early Barremian, Palorbitolina assemblage = Late Barremian-Early Aptian, Mesorbitolina assemblage = Late Aptian). The identified taxa are dominated by agglutinating larger benthic foraminifera including Eopalorbitolina, Palorbitolina, Mesorbitolina, Orbitolinopsis, Dictyoconus, Paleodictyoconus, Vercorsella, Mayncina, Charrentia, Trocholina and Pseudolituonella." @default.
- W2181815500 created "2016-06-24" @default.
- W2181815500 creator A5011116164 @default.
- W2181815500 creator A5024080335 @default.
- W2181815500 date "2010-01-01" @default.
- W2181815500 modified "2023-09-24" @default.
- W2181815500 title "Lower Cretaceous Agglutinating Larger Benthic Foraminifera from the Sarvestan Section, south of Esfahan, Iran" @default.
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