SEQUENCE STRATIGRAPHY, SEDIMENTARY ENVIRONMENT IN BAHRAM FORMATION IN SHURAB MOUNTAIN

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TAHERI P.; MOUSAVI S.M.J.; HALAJI M.

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Journal: JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK Year:2009 | Volume:2 | Issue:6 Page(s): 33-44

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Title

SEQUENCE STRATIGRAPHY, SEDIMENTARY ENVIRONMENT IN BAHRAM FORMATION IN SHURAB MOUNTAIN

Author(s)

TAHERI P. | MOUSAVI S.M.J. | HALAJI M. | Issue Writer Certificate

Keywords

BAHRAM FORMATIONQ2

SEDIMENTARY ENVIRONMENTSQ3

SEQUENCE STRATIGRAPHYQ2

Abstract

In order to study SEQUENCE STRATIGRAPHY, facies and depositional environment of Bahram (Devonian) Formation, a stratigraphic section with a thickness of 368 m in Mountain.Shurab, located in southern Damghan, was selected. This Formation Consist Mainly Of Carbonate And Dolomite Facies. Microscopic studies of BAHRAM FORMATION led to the recognition of four Facies Groups, coastal subenvironment, tidal flat, lagoonal and shoal. Coastal facies consist of three microfacies: sublitarnite, quartzarnite and calclitite. Tidal flat facies consist of stromatolite boundstone and lime mudstone. Lagoonal facies consist of bioclast wackestone, peloidal bioclast grainstone, peloidal bioclast packstone and umbella/osteracoda packstone. Finally, shoal facies include bioclast packstone/grainstone microfacies. This Formation was depositional in a ramp sequence. Microfacies vertical changes and their comparison with sea level fluctuations led to the distinction of three large-scale sedimentary sequences.The first sequence is contain TST and HST para sequences upper part of this sequence is of type SB2. secondary sequence begin with alternative of thin limestone belong tidal flat (TST) environment that upward change to dolomite and thick beded limestone. Maximum flooding surface is located in Bioclactic grainstone facies. Hrid sequence is contain TST and HST. The upper boundary of Third sequence is of type SB2.

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APA: Copy

TAHERI, P., MOUSAVI, S.M.J., & HALAJI, M.. (2009). SEQUENCE STRATIGRAPHY, SEDIMENTARY ENVIRONMENT IN BAHRAM FORMATION IN SHURAB MOUNTAIN. JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, 2(6), 33-44. SID. https://sid.ir/paper/357951/en

Vancouver: Copy

TAHERI P., MOUSAVI S.M.J., HALAJI M.. SEQUENCE STRATIGRAPHY, SEDIMENTARY ENVIRONMENT IN BAHRAM FORMATION IN SHURAB MOUNTAIN. JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK[Internet]. 2009;2(6):33-44. Available from: https://sid.ir/paper/357951/en

IEEE: Copy

P. TAHERI, S.M.J. MOUSAVI, and M. HALAJI, “SEQUENCE STRATIGRAPHY, SEDIMENTARY ENVIRONMENT IN BAHRAM FORMATION IN SHURAB MOUNTAIN,” JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, vol. 2, no. 6, pp. 33–44, 2009, [Online]. Available: https://sid.ir/paper/357951/en

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