DEPOSITIONAL ENVIRONMENTS AND SEQUENCE STRATIGRAPHY OF KAZHDUMI AND SARVAK FORMATIONS IN FARS PROVINCE (KANGAN SURFACE SECTION AND BUZPAR SUB SURFACE NO.1) SW IRAN

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TABATABAEI PARISA; LASEMI YAGHOOB; JAHANI DAVOOD; KOHANSAL GHADIMVAND NADER

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Journal: JOURNAL OF THE EARTH Year:2010 | Volume:5 | Issue:3 Page(s): 131-144

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Title

DEPOSITIONAL ENVIRONMENTS AND SEQUENCE STRATIGRAPHY OF KAZHDUMI AND SARVAK FORMATIONS IN FARS PROVINCE (KANGAN SURFACE SECTION AND BUZPAR SUB SURFACE NO.1) SW IRAN

Author(s)

TABATABAEI PARISA | LASEMI YAGHOOB | JAHANI DAVOOD | KOHANSAL GHADIMVAND NADER | Issue Writer Certificate

Keywords

FACIESQ2

DEPOSITIONAL ENVIRONMENTQ2

DEPOSITIONAL MODELQ2

RAMPQ2

SEQUENCE STRATIGRAPHYQ2

Abstract

The Bangestan Group (Middle-Upper Cretaceous) in southwest Iran includes Kazhdumi, Sarvak and Ilam formations. To study FACIES, DEPOSITIONAL ENVIRONMENTs and SEQUENCE STRATIGRAPHY of Kazhdumi and Sarvak formations in Fars area, stratigraphic sections of Buzpar well no.1 (Kazhdumi and Sarvak formations), Namak Kangan (Kazhdumi Formation) and Kangan (Sarvak Formation) have been studied.FACIES studies of the Kazhdumi Formation led to recognition of siliciclastic and carbonate FACIES. Sandstones of the Kazhdumi Formation (Quartzarenite) were probably deposited in a beach environment. Carbonate FACIES of Kazhdumi and Sarvak formations were deposited in open marine (A), barrier (B), lagoon (C) and lower intertidal (D) FACIES belt.FACIES types and their vertical changes and comparision with recent and ancient DEPOSITIONAL ENVIRONMENTs indicate that the FACIES of the Kazhdumi and Sarvak formations were deposited in a RAMP platform.Sequence stratigraphy indicates that Kazhdumi and Sarvak formations in Coastal Fars include two depositional sequences and in Sub-Coastal Fars consist of three depositional sequences. The first sequence (Upper Albian- Lower Cenomanian) in Kangan and Buzpar sections (Coastal Fars and sub- Coastal Fars) includes the Kazhdumi Formation and the lower part of the Sarvak Formation (Lower Madod). The lower boundary of first sequence is a type 1 sequence boundary (SB1). The second sequence (Lower-Middle Cenomanian) includes the middle part of the Sarvak Formation. The contact between the first and second sequence is type 2 sequence boundary (SB2). The upper limit of the second sequence is the laterite horizone related to Cenomanian- Torunian unconformity in Kangan section. The third sequence (Middle Cenomanian) include the upper part of the Sarvak Formation in Buzpar well no.1. The lower boundary of third sequence is a type 2 sequence boundary (SB2) and the upper boundary of this sequence is a type 1 sequence boundary (SB1).

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APA: Copy

TABATABAEI, PARISA, LASEMI, YAGHOOB, JAHANI, DAVOOD, & KOHANSAL GHADIMVAND, NADER. (2010). DEPOSITIONAL ENVIRONMENTS AND SEQUENCE STRATIGRAPHY OF KAZHDUMI AND SARVAK FORMATIONS IN FARS PROVINCE (KANGAN SURFACE SECTION AND BUZPAR SUB SURFACE NO.1) SW IRAN. JOURNAL OF THE EARTH, 5(3), 131-144. SID. https://sid.ir/paper/192984/en

Vancouver: Copy

TABATABAEI PARISA, LASEMI YAGHOOB, JAHANI DAVOOD, KOHANSAL GHADIMVAND NADER. DEPOSITIONAL ENVIRONMENTS AND SEQUENCE STRATIGRAPHY OF KAZHDUMI AND SARVAK FORMATIONS IN FARS PROVINCE (KANGAN SURFACE SECTION AND BUZPAR SUB SURFACE NO.1) SW IRAN. JOURNAL OF THE EARTH[Internet]. 2010;5(3):131-144. Available from: https://sid.ir/paper/192984/en

IEEE: Copy

PARISA TABATABAEI, YAGHOOB LASEMI, DAVOOD JAHANI, and NADER KOHANSAL GHADIMVAND, “DEPOSITIONAL ENVIRONMENTS AND SEQUENCE STRATIGRAPHY OF KAZHDUMI AND SARVAK FORMATIONS IN FARS PROVINCE (KANGAN SURFACE SECTION AND BUZPAR SUB SURFACE NO.1) SW IRAN,” JOURNAL OF THE EARTH, vol. 5, no. 3, pp. 131–144, 2010, [Online]. Available: https://sid.ir/paper/192984/en

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