STUDY OF ICHNOFOSSILS AND ICHNOFACIES OF THE
UPPER PART OF THE SHEMSHAK FORMATION AT
TAZAREHAREA (NORTH EAST DAMGHAN)

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MOGHADDAM H.V.; TAHERI A.A.GH.

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Journal: GEOSCIENCES Year:2004 | Volume:11 | Issue:51-52 Page(s): 46-57

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Information Journal Paper

Title

STUDY OF ICHNOFOSSILS AND ICHNOFACIES OF THE UPPER PART OF THE SHEMSHAK FORMATION AT TAZAREHAREA (NORTH EAST DAMGHAN)

Author(s)

MOGHADDAM H.V. | TAHERI A.A.GH. | Issue Writer Certificate

Keywords

ICHNOFOSSILSQ4

ICHNOFACIESQ2

SHEMSHAK F.Q4

TAZAREHQ4

DAMGHANQ2

IRANQ2

Abstract

The upper part of the SHEMSHAK F.rmation at TAZAREH area consists of sandstone, siltstone, and shale beds with marine fossils.Based on systematic study of the ICHNOFOSSILS in these sediments, 9 ichnogenera, in two assemblages have been identified. The first assemblage with low ichnodiversity (Skolithos, Arenicolites, Diplocraterion) occurs in the siltstone and sandstonebeds. This assemblage ofichnofauna represents the skolithos ICHNOFACIES which formed in a relatively high energy condition. The second assemblage with higher ichnodiversity (Planolites, Palaeophycus, Neonerites, Cochlichnus, Rhizocorallium,Chondrites) is very common in the shale beds. This assemblage represents the cruziana ICHNOFACIES which formedin a relatively lower energy condition.

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APA: Copy

MOGHADDAM, H.V., & TAHERI, A.A.GH.. (2004). STUDY OF ICHNOFOSSILS AND ICHNOFACIES OF THE UPPER PART OF THE SHEMSHAK FORMATION AT TAZAREHAREA (NORTH EAST DAMGHAN). GEOSCIENCES, 11(51-52), 46-57. SID. https://sid.ir/paper/358742/en

Vancouver: Copy

MOGHADDAM H.V., TAHERI A.A.GH.. STUDY OF ICHNOFOSSILS AND ICHNOFACIES OF THE UPPER PART OF THE SHEMSHAK FORMATION AT TAZAREHAREA (NORTH EAST DAMGHAN). GEOSCIENCES[Internet]. 2004;11(51-52):46-57. Available from: https://sid.ir/paper/358742/en

IEEE: Copy

H.V. MOGHADDAM, and A.A.GH. TAHERI, “STUDY OF ICHNOFOSSILS AND ICHNOFACIES OF THE UPPER PART OF THE SHEMSHAK FORMATION AT TAZAREHAREA (NORTH EAST DAMGHAN),” GEOSCIENCES, vol. 11, no. 51-52, pp. 46–57, 2004, [Online]. Available: https://sid.ir/paper/358742/en

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