The Upper Triassic Nayband Formation is located in eastern central Iran and preserves events such as the Eo-Cimmerian. The rocks of this formation are composed of detrital carbonate-silica sediments.Sandstone petrography and geochemistry of the Nayband Formation (Upper Triassic, Central Iran): Implications for sediment provenance and tectonic settingSedimentary environment and provenance of sandstones from the Qadir member in the Nayband Formation, Tabas block, east-central Iran
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