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Information Journal Paper

Title

BIOSTRTIGRAPHY AND PALEOECOLOGY OF UPPER CRETACEOUS DEPOSITS IN HONOOJ SECTION (WEST OF KERMAN)

Pages

  93-108

Abstract

 The Upper Cretaceous thick bedded succession in BADAMOUYEH MOUNTAIN in HONOOJ area shows the LATE CENOMANIAN-SANTONIAN stages. Also, these deposits are well exposed in south-west of Bibihayat and south of Cheshmah Gaz village. In the studied section, Lower and Upper HONOOJ green marls (informal) with intercalation of EXOGYROFEROUS SHALY LIMESTONE are overlain by thick bedded limestones and in turns disconformably cover the Jurassic shale and sandstones (probably Hojedk Formation). The presences of both PLATYCOPID and PODOCOPID ostracods, high diverse assemblages of foraminifera and macrofossils in HONOOJ marls and also high diverse assemblages of benthonic foraminifera in upper limestone show a favorable condition during the deposition of the strata.

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    Cite

    APA: Copy

    LOTF ABAD ARAB, A., & VAZIRI, M.R.. (2011). BIOSTRTIGRAPHY AND PALEOECOLOGY OF UPPER CRETACEOUS DEPOSITS IN HONOOJ SECTION (WEST OF KERMAN). SEDIMENTARY FACIES, 4(1), 93-108. SID. https://sid.ir/paper/199858/en

    Vancouver: Copy

    LOTF ABAD ARAB A., VAZIRI M.R.. BIOSTRTIGRAPHY AND PALEOECOLOGY OF UPPER CRETACEOUS DEPOSITS IN HONOOJ SECTION (WEST OF KERMAN). SEDIMENTARY FACIES[Internet]. 2011;4(1):93-108. Available from: https://sid.ir/paper/199858/en

    IEEE: Copy

    A. LOTF ABAD ARAB, and M.R. VAZIRI, “BIOSTRTIGRAPHY AND PALEOECOLOGY OF UPPER CRETACEOUS DEPOSITS IN HONOOJ SECTION (WEST OF KERMAN),” SEDIMENTARY FACIES, vol. 4, no. 1, pp. 93–108, 2011, [Online]. Available: https://sid.ir/paper/199858/en

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