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Publikováno v:
Journal of Stratigraphy and Sedimentology Researches, Vol 32, Iss 4, Pp 29-46 (2016)
Introduction The siliciclastic sediments of Kashafrud Formation (Bajocian–Bathonian) in the Kopet-Dagh Basin (Madani, 1977; Afshar-Harb, 1979) are composed of conglomerate, sandstone and shale. It is reported that these sediments were mostly deposi
Externí odkaz:
https://doaj.org/article/48769a71d7ab4a9d983cb99198735e28
