The Upper Triassic (Norian–Rhaetian) Nayband Formation is situated at the southwestern margin of Central East Iranian Microcontinent and records Eo-Cimmerian events. The formation is composed of mixed carbonate-siliciclastic deposits.[1][2][3][4]

References

  1. ^ Sabbaghiyan, Hossein; Aria-Nasab, Mohammadreza; Ghasemi-Nejad, Ebrahim (2020-11-01). "The palynology of the Nayband Formation (Upper Triassic) of the Tabas Block, Central Iran". Review of Palaeobotany and Palynology. 282: 104308. doi:10.1016/j.revpalbo.2020.104308. ISSN 0034-6667.
  2. ^ Sandstone petrography and geochemistry of the Nayband Formation (Upper Triassic, Central Iran): Implications for sediment provenance and tectonic setting
  3. ^ Ghasemi-Nejad, Ebrahim; Agha-Nabati, Ali; Dabiri, Omid (2004-12-01). "Late Triassic dinoflagellate cysts from the base of the Shemshak Group in north of Alborz Mountains, Iran". Review of Palaeobotany and Palynology. 132 (3): 207–217. doi:10.1016/j.revpalbo.2004.07.001. ISSN 0034-6667.
  4. ^ Sedimentary environment and provenance of sandstones from the Qadir member in the Nayband Formation, Tabas block, east-central Iran
Allikas: https://en.wikipedia.org/wiki/Nayband_Formation
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