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Information Journal Paper

Title

THE STUDY OF DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF SARVAK FORMATION IN NORTHERN SHIRAZ (FARS PROVINCE)

Pages

  63-72

Abstract

 In this research two sections of SARVAK FORMATION called Kareh-tavy and Zakiyan totally 585 m including 400 thin sections of upper Cenomanian sediment were selected. The major microFACIES in the studied section include wackestone, packstone, grainstone, boundstone, floatstone and rudstone. These microFACIES fall into four environment groups: open marine, bar, lagoon and tidal areas. The major elements of microFACIES include bioclast, intraclast, extraclast and pleiod.Considering SEQUENCE STRATIGRAPHY studies, two 3rd-order sediment sequences (3rd class cycle) have been identified: sequence 1 (upper Albian to Lower Cenomanian) which is related to Lower Sarvak Farmation, and sequence 2 (Middle to Upper Cenomanian) which is related to middle and upper part of SARVAK FORMATION and include bar, lagoon, tidal flat FACIES.

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    • Cite

    APA: Copy

    AHMADI, V., & MAJDI, M.. (2009). THE STUDY OF DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF SARVAK FORMATION IN NORTHERN SHIRAZ (FARS PROVINCE). JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, 2(5), 63-72. SID. https://sid.ir/paper/186814/en

    Vancouver: Copy

    AHMADI V., MAJDI M.. THE STUDY OF DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF SARVAK FORMATION IN NORTHERN SHIRAZ (FARS PROVINCE). JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK[Internet]. 2009;2(5):63-72. Available from: https://sid.ir/paper/186814/en

    IEEE: Copy

    V. AHMADI, and M. MAJDI, “THE STUDY OF DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF SARVAK FORMATION IN NORTHERN SHIRAZ (FARS PROVINCE),” JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, vol. 2, no. 5, pp. 63–72, 2009, [Online]. Available: https://sid.ir/paper/186814/en

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