Oolitic facies analyses of Badamu Formation at the southeast of Kerman, south of Tabas block: a pattern of beach and beach ridges

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ZAND MOGHADAM H.

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

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Journal: GEOSCIENCES Year:2018 | Volume:27 | Issue:108 Page(s): 83-94

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Title

Oolitic facies analyses of Badamu Formation at the southeast of Kerman, south of Tabas block: a pattern of beach and beach ridges

Author(s)

ZAND MOGHADAM H. | Issue Writer Certificate

Keywords

Oolitic facies analysesQ1

Beach environmentQ1

Badamu FormationQ2

Middle-Upper JurassicQ1

SE KermanQ1

Abstract

The Badamu Formation with Middle-Upper Jurassic (late Toarcian-Early Bajocian) age introduced as the third the formation of Shemshak Group in the Central Iran that for facies studies and depositional environment, the Bolbolueih section in SE Kerman with a thickness 144m was selected and sampled. Facies analyses of the Badamu Formation led to identification of 16 lithofacies that were classified into four facies associations including carbonate, siliciclastic, hetrolithic carbonate-siliciclastic and oolithic ironstone. The important facies of the Badamu Formation in studied section is oolitic calcarenaite facies (La) that according to textural and structural features classified into six lithofacies (Lah, Lal, Lap, Lam, Lar and Lat). The sorted ooides in grainstone microfacies accompanied by structural evidences such as cross-bedding with bimodal to bipolar palaeocurents, hummocky and herringbone cross-beds, reactivation surfaces, wavy ripple marks and rain drop imprints reveal that this facies were deposited in shallow Beach environment. Textural and structural characterizes in the associated facies (sandstone and hetrolitic fasies) such as high textural and compositional maturity and flaser bedding is consistent with this interpretation. Vertical and lateral accretions of the recognized facies show that the Badamu Formation successions have been deposited in a shoreface subenvironment in the beach and beach ridges model framework.

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APA: Copy

ZAND MOGHADAM, H.. (2018). Oolitic facies analyses of Badamu Formation at the southeast of Kerman, south of Tabas block: a pattern of beach and beach ridges. GEOSCIENCES, 27(108 ), 83-94. SID. https://sid.ir/paper/32534/en

Vancouver: Copy

ZAND MOGHADAM H.. Oolitic facies analyses of Badamu Formation at the southeast of Kerman, south of Tabas block: a pattern of beach and beach ridges. GEOSCIENCES[Internet]. 2018;27(108 ):83-94. Available from: https://sid.ir/paper/32534/en

IEEE: Copy

H. ZAND MOGHADAM, “Oolitic facies analyses of Badamu Formation at the southeast of Kerman, south of Tabas block: a pattern of beach and beach ridges,” GEOSCIENCES, vol. 27, no. 108 , pp. 83–94, 2018, [Online]. Available: https://sid.ir/paper/32534/en

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