Nayband Formation
| Nayband Formation | |
|---|---|
| Stratigraphic range: | |
| Type | Geological formation |
| Lithology | |
| Primary | Mainly siliciclastic; Shale, sandstone, Mudrock |
| Other | siltstone, Coal |
| Location | |
| Region | Kerman Province, |
| Country | Iran |
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.[1][2][3][4]
References
[edit]- ^ 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.
- ^ Sandstone petrography and geochemistry of the Nayband Formation (Upper Triassic, Central Iran): Implications for sediment provenance and tectonic setting
- ^ 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.
- ^ Sedimentary environment and provenance of sandstones from the Qadir member in the Nayband Formation, Tabas block, east-central Iran
 | This article about a specific stratigraphic formation is a stub. You can help Wikipedia by expanding it. |
 | This Iran-related article is a stub. You can help Wikipedia by expanding it. |