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ABBASSI, N.. (1386). SHALLOW MARINE TRACE FOSSILS FROM UPPER DEVONIAN SEDIMENTS OF THE KUH-E ZARD, ZEFREH AREA, CENTRAL IRAN. , 31(1), 23-33. doi: 10.22099/ijsts.2007.2313
N. ABBASSI. "SHALLOW MARINE TRACE FOSSILS FROM UPPER DEVONIAN SEDIMENTS OF THE KUH-E ZARD, ZEFREH AREA, CENTRAL IRAN". , 31, 1, 1386, 23-33. doi: 10.22099/ijsts.2007.2313
ABBASSI, N.. (1386). 'SHALLOW MARINE TRACE FOSSILS FROM UPPER DEVONIAN SEDIMENTS OF THE KUH-E ZARD, ZEFREH AREA, CENTRAL IRAN', , 31(1), pp. 23-33. doi: 10.22099/ijsts.2007.2313
ABBASSI, N.. SHALLOW MARINE TRACE FOSSILS FROM UPPER DEVONIAN SEDIMENTS OF THE KUH-E ZARD, ZEFREH AREA, CENTRAL IRAN. , 1386; 31(1): 23-33. doi: 10.22099/ijsts.2007.2313

SHALLOW MARINE TRACE FOSSILS FROM UPPER DEVONIAN SEDIMENTS OF THE KUH-E ZARD, ZEFREH AREA, CENTRAL IRAN

Iranian Journal of Science
مقاله 4، دوره 31، شماره 1، اردیبهشت 2007، صفحه 23-33    اصل مقاله (559.45 K)
نوع مقاله: Regular Paper
شناسه دیجیتال (DOI): 10.22099/ijsts.2007.2313
نویسنده
N. ABBASSI*
Department of Geology, Faculty of Sciences, Zanjan University, Zanjan 45171, I. R. of Iran
چکیده
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
کلیدواژه‌ها
Trace fossils؛ Systematic ichnology؛ Upper Devonian؛ Central Iran
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