Sedimentary environment, sequence stratigraphy and elemental geochemistry of the Taleh Zang Formation in the South of Kermanshah

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Shalalvand Mohammad; ADABI MOHAMMAD HOSSEIN; ZOHDI AFSHIN

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Journal: JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES Year:2019 | Volume:35 | Issue:2 (75) Page(s): 25-48

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Title

Sedimentary environment, sequence stratigraphy and elemental geochemistry of the Taleh Zang Formation in the South of Kermanshah

Author(s)

Shalalvand Mohammad | ADABI MOHAMMAD HOSSEIN | ZOHDI AFSHIN | Issue Writer Certificate

Keywords

Taleh Zang FormationQ2

Sedimentary EnvironmentQ2

Sequence StratigraphyQ2

Elemental GeochemistryQ2

KermanshahQ1

Abstract

In this study, for the first time depositional conditions, Sequence Stratigraphy and Elemental Geochemistry of the Taleh Zang Formation with Paleocene to Lower Eocene age in the Kermanshah province (Kaboutar Bala section) have been evaluated. In this section, the Taleh Zang Formation conformably overlies the Amiran Formation and is overlain by the Kashkan Formation with a disconformity surface. Field and microscopic studies led to recognition of six microfacies within the succession. Gradual microfacies change, the absence of calciturbidites and lack of extensive barrier reefs with considerable thickness, confirms a carbonate ramp. Sequence stratigraphic studies led to the identification of one-third order depositional sequence which includes TST and HST facies association. The lower boundary of this sequence, specified as type II and the upper boundary with evidences of subaerial exposure is type I. The maximum flooding surface (MFS) is determined with bioclastic coral corallinacea floatstone/rudstone microfacies of proximal middle ramp. The results of geochemical analysis of major elements (Ca, Mg) and minor elements (Sr, Na, Mn and Fe) indicate that the original carbonate mineralogy is aragonite and diagenetic system is semi-close to open system. Trend of elements changes along this stratigraphic section shows that in the HST sediments, the amount of Sr is decreased, while Fe and Mn are increased due to more meteoric diagenetic effect.

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APA: Copy

Shalalvand, Mohammad, ADABI, MOHAMMAD HOSSEIN, & ZOHDI, AFSHIN. (2019). Sedimentary environment, sequence stratigraphy and elemental geochemistry of the Taleh Zang Formation in the South of Kermanshah. JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES, 35(2 (75) ), 25-48. SID. https://sid.ir/paper/157023/en

Vancouver: Copy

Shalalvand Mohammad, ADABI MOHAMMAD HOSSEIN, ZOHDI AFSHIN. Sedimentary environment, sequence stratigraphy and elemental geochemistry of the Taleh Zang Formation in the South of Kermanshah. JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES[Internet]. 2019;35(2 (75) ):25-48. Available from: https://sid.ir/paper/157023/en

IEEE: Copy

Mohammad Shalalvand, MOHAMMAD HOSSEIN ADABI, and AFSHIN ZOHDI, “Sedimentary environment, sequence stratigraphy and elemental geochemistry of the Taleh Zang Formation in the South of Kermanshah,” JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES, vol. 35, no. 2 (75) , pp. 25–48, 2019, [Online]. Available: https://sid.ir/paper/157023/en

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