作者: M. Javanbakht , S. Ghazi , R. Moussavi-Harami , A. Mahboubi
DOI: 10.1007/S12594-013-0208-2
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摘要: The Tirgan Formation (Barremian — Aptian) is exposed in the Kopet Dagh northeast Iran. Two stratigraphic sections Radkan and Chenaran were measured. Their thickness are 238 m 119 m, respectively. This formation measured consists of three parts (including lower carbonate, middle limy shale marl upper carbonate rocks). Based on study 164 thin-sections, 15 2 siliciclastic lithofacies have been identified. Carbonate deposited a ramp platform fore shoal, lagoon tidal flat environments. Sea level changes during Cretaceous led to different large-scale depositional sequences (two) present highlights reconstruction tectonic history area Cretaceous.