ISSN 1543-8740
Vol. 19, Issue 1, 2021February 24, 2021 CDT
Facies changes and a major negative d13C shift suggest the base of Mila Formation as the likely base of the Miaolingian Series, Alborz Mountains, northern Iran
Facies changes and a major negative d13C shift suggest the base of Mila Formation as the likely base of the Miaolingian Series, Alborz Mountains, northern Iran
Articles in Vol. 19, Issue 1, 2021
Vol. 19, Issue 1, 2021
- Renovation of _The Sedimentary Record_Jenn PickeringJeong-Hyun Lee
- Addressing a Phanerozoic carbonate facies conundrum—sponges or clotted micrite? Evidence from Early Silurian reefs, South China BlockStephen KershawQijian LiYue Li
- Facies changes and a major negative d13C shift suggest the base of Mila Formation as the likely base of the Miaolingian Series, Alborz Mountains, northern IranHadi Amin-RasouliYaghoob Lasemi
Amin-Rasouli, Hadi, and Yaghoob Lasemi. 2021. “Facies Changes and a Major Negative d13C Shift Suggest the Base of Mila Formation as the Likely Base of the Miaolingian Series, Alborz Mountains, Northern Iran.” The Sedimentary Record 19 (1): 11–14. https://doi.org/10.2110/sedred.2021.1.04.