PALEONTOLOGY AND PALEOENVIRONMENT OF TARBUR FORMATION IN KHORRAMABAD AREA

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MAGHFOURI MOGHADAM I.

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Journal: GEOSCIENCES Year:2006 | Volume:15 | Issue:58 Page(s): 38-45

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Title

PALEONTOLOGY AND PALEOENVIRONMENT OF TARBUR FORMATION IN KHORRAMABAD AREA

Author(s)

MAGHFOURI MOGHADAM I. | Issue Writer Certificate

Keywords

TETHYSQ2

TARBURQ2

KHORRAMABADQ2

MAESTRICHTIANQ2

Abstract

During Campanian-Maestrichtian an association of Rudist-rich thrived sedimet was formed along the south eastern NeoTETHYS margin. This rock unit is called TARBUR Formation in the Zagros mountains. The main extension of the formation is in the interior Fars; however, it has slim outcrops in KHORRAMABAD area. TARBUR Formation conformably overlies Amiran Formation and is disconformably underlain by the Kashkan Formation. Paleontological study indicates that the age of TARBUR Formation in the study area is the Middle MAESTRICHTIAN. Facies analysis and petrographic study led to the recognition of four microfacies of the low-angle open shelf margin. Furthermore, this formation was deposited during a regressive phase in a warm and low energy shallow marine environment.

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ریف رودیستی کرتاسه فوقانی در پلاتفرم کم عمق کربناته شرق حوضه کپه داغ

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APA: Copy

MAGHFOURI MOGHADAM, I.. (2006). PALEONTOLOGY AND PALEOENVIRONMENT OF TARBUR FORMATION IN KHORRAMABAD AREA. GEOSCIENCES, 15(58), 38-45. SID. https://sid.ir/paper/32586/en

Vancouver: Copy

MAGHFOURI MOGHADAM I.. PALEONTOLOGY AND PALEOENVIRONMENT OF TARBUR FORMATION IN KHORRAMABAD AREA. GEOSCIENCES[Internet]. 2006;15(58):38-45. Available from: https://sid.ir/paper/32586/en

IEEE: Copy

I. MAGHFOURI MOGHADAM, “PALEONTOLOGY AND PALEOENVIRONMENT OF TARBUR FORMATION IN KHORRAMABAD AREA,” GEOSCIENCES, vol. 15, no. 58, pp. 38–45, 2006, [Online]. Available: https://sid.ir/paper/32586/en

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