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Information Journal Paper

Title

FACIES AND DEPOSITIONAL ENVIRONMENT OF THE RUTEH FORMATION IN THE NORTH OF SHAHROUD (EASTERN ALBORZ)

Pages

  73-85

Abstract

 The deposits of the RUTEH FORMATION (Upper PERMIAN) in the north of Shahroud (Ghatar Seresht valley) are 187.34 meters thick.It is unconformably overlain by the Doroud Formation (Lower PERMIAN) and is unconformably underlain by the Elika Formation (Triassic) with a thick laterite horizon. In this section, the RUTEH FORMATION consists of limestone with shale lime interbedded in the lower part, fossiliferous limestone with marl lime in the middle part, and a period of thick layer oncoidal limestone and marl lime in the upper part. Field and microscopic studies of the RUTEH FORMATION led to the recognition of one FACIES group of full carbonate. The carbonate FACIES consists of 22 FACIES including 4 FACIES groups related to tidal flat, lagoon, barrier, and open marine. The carbonate FACIES group has been deposited in a homoclinal ramp.

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    APA: Copy

    JAVAD MOUSAVI, SEYED MOHAMMAD, & NOROUZI, ENSIEH. (2009). FACIES AND DEPOSITIONAL ENVIRONMENT OF THE RUTEH FORMATION IN THE NORTH OF SHAHROUD (EASTERN ALBORZ). JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, 2(4), 73-85. SID. https://sid.ir/paper/186834/en

    Vancouver: Copy

    JAVAD MOUSAVI SEYED MOHAMMAD, NOROUZI ENSIEH. FACIES AND DEPOSITIONAL ENVIRONMENT OF THE RUTEH FORMATION IN THE NORTH OF SHAHROUD (EASTERN ALBORZ). JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK[Internet]. 2009;2(4):73-85. Available from: https://sid.ir/paper/186834/en

    IEEE: Copy

    SEYED MOHAMMAD JAVAD MOUSAVI, and ENSIEH NOROUZI, “FACIES AND DEPOSITIONAL ENVIRONMENT OF THE RUTEH FORMATION IN THE NORTH OF SHAHROUD (EASTERN ALBORZ),” JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, vol. 2, no. 4, pp. 73–85, 2009, [Online]. Available: https://sid.ir/paper/186834/en

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