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:

1,138
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

LITHOSTRATIGRAPHY AND BIOSTRATIGRAPHY OF THE ASMARI FORMATION IN SOUTHERN FLANK OF MISH ANTICLINE (TANG-E-GANAVEH)

Pages

  63-76

Keywords

OLIGOCENE (RUPELIAN-CHATIAN)Q1
EARLY MIOCENE (AQUITANIAN-BURDIGALIAN)Q1

Abstract

 The ASMARI FORMATION in the southern flank of MISH ANTICLINE (in the north of Gachsaran) with a total thickness of 366 m is mainly composed of medium to thick limestone layers. Based on lithological studies, it is mainly composed of a periodic arrangement of marly limestone with very thick, thick and medium bedded limestone layers and in some parts it consists of dolomitic layers.The lower contact of the ASMARI FORMATION with Pabdeh Formation is gradual and its upper contact with the Gachsaran Formation is conformable with some sharp lithological changes. Based on change in thickness of layers, color and lithology, this carbonate sequence is subdivided into three lithological units.In Biostratigraphic studies, 28 species belonging to 41 genera of foraminifera were recognized. According to recognized biozone and foraminifera assemblages, 4 biozones and one undetermined zone were classified according to Laursen et al., 2009. The age of the ASMARI FORMATION in this section is Oligocene (Rupelian-Chatian) to Early Miocene (Aquitanian-Bourdigalian).

Cites

  • No record.
  • References

  • No record.
  • Cite

    APA: Copy

    MORADI, F., SADEGHI, A., AMIRI BAKHTIAR, H., & ALLAHKARAMPOUR DILL, M.. (2016). LITHOSTRATIGRAPHY AND BIOSTRATIGRAPHY OF THE ASMARI FORMATION IN SOUTHERN FLANK OF MISH ANTICLINE (TANG-E-GANAVEH). IRANIAN JOURNAL OF GEOLOGY, 10(37), 63-76. SID. https://sid.ir/paper/129400/en

    Vancouver: Copy

    MORADI F., SADEGHI A., AMIRI BAKHTIAR H., ALLAHKARAMPOUR DILL M.. LITHOSTRATIGRAPHY AND BIOSTRATIGRAPHY OF THE ASMARI FORMATION IN SOUTHERN FLANK OF MISH ANTICLINE (TANG-E-GANAVEH). IRANIAN JOURNAL OF GEOLOGY[Internet]. 2016;10(37):63-76. Available from: https://sid.ir/paper/129400/en

    IEEE: Copy

    F. MORADI, A. SADEGHI, H. AMIRI BAKHTIAR, and M. ALLAHKARAMPOUR DILL, “LITHOSTRATIGRAPHY AND BIOSTRATIGRAPHY OF THE ASMARI FORMATION IN SOUTHERN FLANK OF MISH ANTICLINE (TANG-E-GANAVEH),” IRANIAN JOURNAL OF GEOLOGY, vol. 10, no. 37, pp. 63–76, 2016, [Online]. Available: https://sid.ir/paper/129400/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