DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF THE FAHLIYAN FORMATION: SURFACE SECTIONS OF BIDKHON AND KHARTANG AND SUBSURFACE SECTIONS OF NAR-2 AND WEST AGHAR

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MALEKI S.; KHOSROW TEHRANI KH.; ASILIAN H.; LASEMI Y.

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Paper Information

Journal: JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY) Year:2009 | Volume:4 | Issue:4 Page(s): 287-298

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Title

DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF THE FAHLIYAN FORMATION: SURFACE SECTIONS OF BIDKHON AND KHARTANG AND SUBSURFACE SECTIONS OF NAR-2 AND WEST AGHAR

Author(s)

MALEKI S. | KHOSROW TEHRANI KH. | ASILIAN H. | LASEMI Y. | Issue Writer Certificate

Keywords

FACIESQ2

DEPOSITIONAL ENVIRONMENTQ4

SEQUENCE STRATIGRAPHYQ3

FAHLIYAN FORMATIONQ3

SOUTHWEST OF FARS BASINQ3

Abstract

The FAHLIYAN FORMATION of the upper Khami Group (Lower Cretaceous) composed of carbonate Rocks. In order to study FACIES, DEPOSITIONAL ENVIRONMENT and SEQUENCE STRATIGRAPHY of the FAHLIYAN FORMATION in the SOUTHWEST OF FARS BASIN, surface sections (Bidkhon in Assaluyeh Anticline and Khartang) and subsurface sections (Nar-2 and West Aghar) have been studied. Field observations and Petrographic studies indicate that the FAHLIYAN FORMATION deposited in four FACIES belts: Tidal Flat (A), Lagoon (B), Barrier (C) and Open marine (D). Study of FACIES, their Vertical and Lateral changes and comparison with modern and ancient environments indicate that the FAHLIYAN FORMATION deposited in a Shelf carbonate platform with shallow environments. SEQUENCE STRATIGRAPHY of the FAHLIYAN FORMATION in the area indicates on the existence of two depositional sequences (3rd-order cycles). In studied sections, lower boundary and top boundary of the first sequence and top boundary of the second sequence are type 1 unconformity (SB1).

Cites

MICROBIOSTRATIGRAPHY AND SEDIMENTARY ENVIRONMENT OF THE SURMEH FORMATION AT GADVAN MOUNTAIN

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APA: Copy

MALEKI, S., KHOSROW TEHRANI, KH., ASILIAN, H., & LASEMI, Y.. (2009). DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF THE FAHLIYAN FORMATION: SURFACE SECTIONS OF BIDKHON AND KHARTANG AND SUBSURFACE SECTIONS OF NAR-2 AND WEST AGHAR. JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY), 4(4), 287-298. SID. https://sid.ir/paper/127107/en

Vancouver: Copy

MALEKI S., KHOSROW TEHRANI KH., ASILIAN H., LASEMI Y.. DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF THE FAHLIYAN FORMATION: SURFACE SECTIONS OF BIDKHON AND KHARTANG AND SUBSURFACE SECTIONS OF NAR-2 AND WEST AGHAR. JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY)[Internet]. 2009;4(4):287-298. Available from: https://sid.ir/paper/127107/en

IEEE: Copy

S. MALEKI, KH. KHOSROW TEHRANI, H. ASILIAN, and Y. LASEMI, “DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF THE FAHLIYAN FORMATION: SURFACE SECTIONS OF BIDKHON AND KHARTANG AND SUBSURFACE SECTIONS OF NAR-2 AND WEST AGHAR,” JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY), vol. 4, no. 4, pp. 287–298, 2009, [Online]. Available: https://sid.ir/paper/127107/en

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