Integrated biostratigraphy (orbitolinids and calcareous nannofossils) of the Lower Cretaceous Taft Formation in Isfahan, Central Iran
The so-called “Upper Orbitolina Limestone” of Isfahan is a relatively thick lithological unit of the Taft Formation, cropping out in Central Iran, that is known for its orbitolinid inventory. An integrated biostratigraphy based on agglutinated benthic foraminifera (mainly orbitolinids) and calcareou...
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Veröffentlicht in: | Cretaceous research 2021-10, Vol.126, p.104918, Article 104918 |
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