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Information Journal Paper

Title

SEDIMENATRY ENVIRONMENTS AND SEQUENCE STRATIGRAPHY OF CARBONIFEROUS SEDIMENTS IN DARCHALEH AREA (NE ESFAHAN)

Pages

  73-83

Abstract

 Carboniferous deposits in DARCHALEH area, 70 km southeast of Esfahan, are 323 meters thick and mainly composed of carbonate and clastic rocks. The lower part of the CARBONIFEROUS strata in this area is covered by alluvial deposits and their upper port is marked by a disconformity with Permian deposits. Based on petrographic and field studies the sediments in this area are belong to 4 sedimentary environments including coastal, tidal flat, lagoon and barrier environments. These environments have been part of a carbonate homoclinal ramp. SEQUENCE STRATIGRAPHY analysis based on Martin- Chivelet method led to the identification of 3, third order depositional sequence that consist of LST, TST and HST. These sequences are bounded by type 1 and 2 sequence boundaries.

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    APA: Copy

    DAVOUDI FARD, Z., KANGAZIYAN, A.H., & SAFARI, A.A.. (2009). SEDIMENATRY ENVIRONMENTS AND SEQUENCE STRATIGRAPHY OF CARBONIFEROUS SEDIMENTS IN DARCHALEH AREA (NE ESFAHAN). JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, 2(6), 73-83. SID. https://sid.ir/paper/186840/en

    Vancouver: Copy

    DAVOUDI FARD Z., KANGAZIYAN A.H., SAFARI A.A.. SEDIMENATRY ENVIRONMENTS AND SEQUENCE STRATIGRAPHY OF CARBONIFEROUS SEDIMENTS IN DARCHALEH AREA (NE ESFAHAN). JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK[Internet]. 2009;2(6):73-83. Available from: https://sid.ir/paper/186840/en

    IEEE: Copy

    Z. DAVOUDI FARD, A.H. KANGAZIYAN, and A.A. SAFARI, “SEDIMENATRY ENVIRONMENTS AND SEQUENCE STRATIGRAPHY OF CARBONIFEROUS SEDIMENTS IN DARCHALEH AREA (NE ESFAHAN),” JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, vol. 2, no. 6, pp. 73–83, 2009, [Online]. Available: https://sid.ir/paper/186840/en

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