CRUZIANA ICHNOFACIES FROM NAYBAND FORMATION (LATE TRIASSIC) IN THE PARVADEH SECTION, SOUTHWEST TABAS, EAST CENTRAL IRAN

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ABBASSI N.; GHAVIDEL SYOOKI M.; YOUSEFI M.; NAVIDI IZAD N.

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Journal: Iranian Journal of Geology Year:2016 | Volume:10 | Issue:38 Page(s): 1-15

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Title

CRUZIANA ICHNOFACIES FROM NAYBAND FORMATION (LATE TRIASSIC) IN THE PARVADEH SECTION, SOUTHWEST TABAS, EAST CENTRAL IRAN

Author(s)

ABBASSI N. | GHAVIDEL SYOOKI M. | YOUSEFI M. | NAVIDI IZAD N. | Issue Writer Certificate

Keywords

CRUZIANA ICHNOFACIESQ2

SEDIMENTARY ENVIRONMENTQ2

LATE TRIASSICQ2

NAYBAND FORMATIONQ2

TABASQ2

Abstract

Nayband Formation is composed of sandstone, coal bearing shales, siltstone, and fossiliferous limestone in the southwest TABAS section, east central Iran. In this section, it is 1410 m in thickness and LATE TRIASSIC in age. A divers trace fossils have been found in the middle parts of sequence as 400-600 m. These trace fossils include Lockeia isp., Palaeophycus tubularis, Palaeophycus striatus, Planolites beverleyensis, Rhizocorallium isp., Rosselia isp., and cf. Treptichnus isp. This ichnoassemblage is attributable to CRUZIANA ICHNOFACIES with presence of Lockeia isp., Rhizocorallium isp., and, Rosselia isp. This part of NAYBAND FORMATION was deposited in low energy conditions below fair-weather wave base.

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APA: Copy

ABBASSI, N., GHAVIDEL SYOOKI, M., YOUSEFI, M., & NAVIDI IZAD, N.. (2016). CRUZIANA ICHNOFACIES FROM NAYBAND FORMATION (LATE TRIASSIC) IN THE PARVADEH SECTION, SOUTHWEST TABAS, EAST CENTRAL IRAN. IRANIAN JOURNAL OF GEOLOGY, 10(38), 1-15. SID. https://sid.ir/paper/129304/en

Vancouver: Copy

ABBASSI N., GHAVIDEL SYOOKI M., YOUSEFI M., NAVIDI IZAD N.. CRUZIANA ICHNOFACIES FROM NAYBAND FORMATION (LATE TRIASSIC) IN THE PARVADEH SECTION, SOUTHWEST TABAS, EAST CENTRAL IRAN. IRANIAN JOURNAL OF GEOLOGY[Internet]. 2016;10(38):1-15. Available from: https://sid.ir/paper/129304/en

IEEE: Copy

N. ABBASSI, M. GHAVIDEL SYOOKI, M. YOUSEFI, and N. NAVIDI IZAD, “CRUZIANA ICHNOFACIES FROM NAYBAND FORMATION (LATE TRIASSIC) IN THE PARVADEH SECTION, SOUTHWEST TABAS, EAST CENTRAL IRAN,” IRANIAN JOURNAL OF GEOLOGY, vol. 10, no. 38, pp. 1–15, 2016, [Online]. Available: https://sid.ir/paper/129304/en

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