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Information Journal Paper

Title

FACIES ANALYSIS AND DEPOSITIONAL MODEL OF UPPER JURASSIC-LOWER CRETACEOUS CARBONATE DEPOSITS IN KHOSRAVAN AREA-CENTRAL ALBORZ

Pages

  125-143

Keywords

Not Registered.

Abstract

 Carbonate deposits of the west of Khosravan village (In Dmavand area) belongs to the Upper Jurassic-Lower Cretaceous. The studied rocks with a thickness of 275 meters are the result of the deposition of laminar to massive carbonates. The lower boundary of the section is continuous and the upper boundary is disconformed. The field and laboratory study of these sediments has led to identifying 5 facies groups including: open marine facies (A), barrier (B), lagoon (C), intertidal (D) and supratidal (E). Comparing the studied facies with ancient and modern environments along with studying the lateral and vertical changes of the facies shows that the mentioned facies in the studied area have been deposited in a carbonated platform of homoclinal ramp type.

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  • References

    Cite

    APA: Copy

    KOHANSAL GHADIMVAND, NADER, & NIKRAVAN MATIN, HOOMAN. (2012). FACIES ANALYSIS AND DEPOSITIONAL MODEL OF UPPER JURASSIC-LOWER CRETACEOUS CARBONATE DEPOSITS IN KHOSRAVAN AREA-CENTRAL ALBORZ. JOURNAL OF THE EARTH, 7(23), 125-143. SID. https://sid.ir/paper/193068/en

    Vancouver: Copy

    KOHANSAL GHADIMVAND NADER, NIKRAVAN MATIN HOOMAN. FACIES ANALYSIS AND DEPOSITIONAL MODEL OF UPPER JURASSIC-LOWER CRETACEOUS CARBONATE DEPOSITS IN KHOSRAVAN AREA-CENTRAL ALBORZ. JOURNAL OF THE EARTH[Internet]. 2012;7(23):125-143. Available from: https://sid.ir/paper/193068/en

    IEEE: Copy

    NADER KOHANSAL GHADIMVAND, and HOOMAN NIKRAVAN MATIN, “FACIES ANALYSIS AND DEPOSITIONAL MODEL OF UPPER JURASSIC-LOWER CRETACEOUS CARBONATE DEPOSITS IN KHOSRAVAN AREA-CENTRAL ALBORZ,” JOURNAL OF THE EARTH, vol. 7, no. 23, pp. 125–143, 2012, [Online]. Available: https://sid.ir/paper/193068/en

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