Upper Devonian sediments of the Kuh-e Zard area northwest of Zefreh, Central Iran, are composed mainly of brown and grey limestones with sandstone and shale intercalations. They contain trace fossils such as Chondrites isp., Diplocraterion parallelum, Fustiglyphus annulatus, Lockeia isp., Phycodes isp., and Taenidium barretti. These trace fossils indicate a shallow marine environment
ABBASSI, N. (2007). SHALLOW MARINE TRACE FOSSILS FROM UPPER DEVONIAN SEDIMENTS OF THE KUH-E ZARD, ZEFREH AREA, CENTRAL IRAN. Iranian Journal of Science, 31(1), 23-33. doi: 10.22099/ijsts.2007.2313
MLA
N. ABBASSI. "SHALLOW MARINE TRACE FOSSILS FROM UPPER DEVONIAN SEDIMENTS OF THE KUH-E ZARD, ZEFREH AREA, CENTRAL IRAN", Iranian Journal of Science, 31, 1, 2007, 23-33. doi: 10.22099/ijsts.2007.2313
HARVARD
ABBASSI, N. (2007). 'SHALLOW MARINE TRACE FOSSILS FROM UPPER DEVONIAN SEDIMENTS OF THE KUH-E ZARD, ZEFREH AREA, CENTRAL IRAN', Iranian Journal of Science, 31(1), pp. 23-33. doi: 10.22099/ijsts.2007.2313
VANCOUVER
ABBASSI, N. SHALLOW MARINE TRACE FOSSILS FROM UPPER DEVONIAN SEDIMENTS OF THE KUH-E ZARD, ZEFREH AREA, CENTRAL IRAN. Iranian Journal of Science, 2007; 31(1): 23-33. doi: 10.22099/ijsts.2007.2313
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