مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Persian Verion

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

video

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

sound

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Persian Version

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

View:

918
مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Download:

0
مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Cites:

Information Journal Paper

Title

DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF THE ASMARI FORMATION IN KUH-E ASMARI AND KUH-E GURPI SURFACE SECTIONS

Pages

  1-24

Abstract

 In this research the sedimentary successions of the ASMARI FORMATION with the age of Oligocene – Miocene in two outcrops of kuh–e Asmari, located in the Dezful embayment with a thickness of 349 m and kuh–e Gurpi (Pabdeh valley), located at the Izeh zone with a thickness of 352m have been studied. The aim of this study is to provide the possibility of comparing Asmari depositional condition in both mentioned area based on lithological studies, determination of microfacies, sedimentary environment and separation of sedimentary sequences. Based on petroghraphic studies, 18 microfacies were identified that were deposited in the three sedimentary environments such as inner ramp, mid ramp and outer ramp. The result of this study showed that Oligo-Miocene carbonates in the kuh–e Asmari section mainly formed in inner ramp environment while in the Pabdeh valley sedimentation occurred in the deeper waters of outer and mid ramp and shallow parts of inner ramp. In the kuh–e Asmari section, sedimentary units shows three third–order depositional sequences, while sequence stratigraphic analysis in the Pabdeh valley shows deposition of the ASMARI FORMATION contains five third–order depositional sequences.

Cites

  • No record.
  • References

  • No record.
  • Cite

    APA: Copy

    DEHGHANZADEH, MAHNAZ, ADABI, MOHAMMAD HOSSEIN, MOUSAVI, MIR REZA, Sadeghi, Abbas, & AVARJANI, SHAHRAM. (2016). DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF THE ASMARI FORMATION IN KUH-E ASMARI AND KUH-E GURPI SURFACE SECTIONS. JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES, 32(1 (62)), 1-24. SID. https://sid.ir/paper/157042/en

    Vancouver: Copy

    DEHGHANZADEH MAHNAZ, ADABI MOHAMMAD HOSSEIN, MOUSAVI MIR REZA, Sadeghi Abbas, AVARJANI SHAHRAM. DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF THE ASMARI FORMATION IN KUH-E ASMARI AND KUH-E GURPI SURFACE SECTIONS. JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES[Internet]. 2016;32(1 (62)):1-24. Available from: https://sid.ir/paper/157042/en

    IEEE: Copy

    MAHNAZ DEHGHANZADEH, MOHAMMAD HOSSEIN ADABI, MIR REZA MOUSAVI, Abbas Sadeghi, and SHAHRAM AVARJANI, “DEPOSITIONAL ENVIRONMENT AND SEQUENCE STRATIGRAPHY OF THE ASMARI FORMATION IN KUH-E ASMARI AND KUH-E GURPI SURFACE SECTIONS,” JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES, vol. 32, no. 1 (62), pp. 1–24, 2016, [Online]. Available: https://sid.ir/paper/157042/en

    Related Journal Papers

    Related Seminar Papers

  • No record.
  • Related Plans

  • No record.
  • Recommended Workshops






    Move to top
    telegram sharing button
    whatsapp sharing button
    linkedin sharing button
    twitter sharing button
    email sharing button
    email sharing button
    email sharing button
    sharethis sharing button