Journal of Geological Research / 2013 / Article / Fig 3

Research Article

Biostratigraphy and Sequence Stratigraphy of Paleogene Deposits in Central Kopet-Dagh Basin (NE of Iran)

Figure 3

(a) Gypsum with radial growth that has been seen in the gradual transition Pesteligh To Chehel-Kaman formations. (b) Cross-laminated. (c) Trace fossils (Thalassinoides) in sandy limestone. (d) Herringbone cross-bedding structure that formed at least two surfaces, and it indicates tidal flat sediments. (e) Horizontal lamination structure in carbonate sequenc. (f) Calcareous Conglomerate that is formed of various grains.

We are committed to sharing findings related to COVID-19 as quickly as possible. We will be providing unlimited waivers of publication charges for accepted research articles as well as case reports and case series related to COVID-19. Review articles are excluded from this waiver policy. Sign up here as a reviewer to help fast-track new submissions.