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Information Journal Paper

Title

FACIES ANALYSIS AND SEDIMENTARY ENVIRONMENT OF THE GADVAN FORMATION IN THE KUZEH KUH ANTICLINE, NORTHEAST OF NURABAD

Pages

  1-12

Abstract

GADVAN FORMATION (Late Barremian to Early Aptian) consists of three members in Kuzeh Kuh section. These members include Lower Gadvan (shale and marl with thin limestone), Khalij limestone and Upper Gadvan (shale and marl with thin limestone). GADVAN FORMATION is 58 meters thick at Kuzeh Kuh section. GADVAN FORMATION is unconformably overlain by Fahlian Formation and conformably overlain by Darian Formation. Field and microscopic investigations of Lower and Upper Gadvan show that these members include shallow open marine benthic foraminifera, shale and marls with planktonic foraminifera and turbidite related to deeper part of this basin. Massive limestone FACIES of Khalij Member show that these sediments were deposited in lagoon and shallow marine environments. GADVAN FORMATION sediments were deposited in a carbonate SHELF platform. The comparison of relative change curve of the studied FACIES with global sea level change shows that GADVAN FORMATION FACIES changing in investigated area corresponds to Arabian platform pattern.

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    APA: Copy

    JAHANI, D., PEYMAN, F., & JAMALI, A.M.. (2009). FACIES ANALYSIS AND SEDIMENTARY ENVIRONMENT OF THE GADVAN FORMATION IN THE KUZEH KUH ANTICLINE, NORTHEAST OF NURABAD. JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, 2(5), 1-12. SID. https://sid.ir/paper/186812/en

    Vancouver: Copy

    JAHANI D., PEYMAN F., JAMALI A.M.. FACIES ANALYSIS AND SEDIMENTARY ENVIRONMENT OF THE GADVAN FORMATION IN THE KUZEH KUH ANTICLINE, NORTHEAST OF NURABAD. JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK[Internet]. 2009;2(5):1-12. Available from: https://sid.ir/paper/186812/en

    IEEE: Copy

    D. JAHANI, F. PEYMAN, and A.M. JAMALI, “FACIES ANALYSIS AND SEDIMENTARY ENVIRONMENT OF THE GADVAN FORMATION IN THE KUZEH KUH ANTICLINE, NORTHEAST OF NURABAD,” JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, vol. 2, no. 5, pp. 1–12, 2009, [Online]. Available: https://sid.ir/paper/186812/en

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