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:

620
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 of the Shahbazan Formation: a tail of evoloving ramp to shelf

Pages

  43-63

Abstract

 The middle-late Eocene Shahbazan Formation is extended in the Lurestan zone. It is underlain by Asmari Formation and overlaying the Kashkan Formation, however to the southwest of the Lurestan, it overlying the Pabdeh Formation with some interfingering lateral changes. Five surface sections and four well which are located in east of the Lurestan zone were sampled to investigate the depositional setting of The Shahbazan Formation. These sections were tentatively selected to survey across and normal to the basin as well. Petrographic examinations on 700 thin sections revealed 17 microfacies which are deposited in tidal flat (3 microfacies), lagoon (4 microfacies), shoal (4 microfacies), reef (1 microfacies) and shallow open marine (5 microfacies). Tidal flat and lagoon facies associations are extended in the north and east, whearas shoal and shallow open marine facies are more frequent in the south and west of the study area. Lack of barrier and also turbidite deposits suggest a NE-SW trending distally steepened ramp in studied area at middle-late Eocene. It is belived that The Shahbazan Formation in Dezful Embayment was deposited on a shelf type carbonate platform in middle Eocene and ramp in late Eocene. This variation could be explained as the consequence of activity of the Mountain Front Fault which was active since late Cretaceous.

Cites

  • No record.
  • References

  • No record.
  • Cite

    APA: Copy

    JANBAZ, M., MOHSENI, H., Piraee, A.R., YOUSEFI YEGANEH, B., & Seradeghi soofiani, h.. (2018). Depositional Environment of the Shahbazan Formation: a tail of evoloving ramp to shelf. APPLIED SEDIMENTOLOGY, 5(10 ), 43-63. SID. https://sid.ir/paper/260580/en

    Vancouver: Copy

    JANBAZ M., MOHSENI H., Piraee A.R., YOUSEFI YEGANEH B., Seradeghi soofiani h.. Depositional Environment of the Shahbazan Formation: a tail of evoloving ramp to shelf. APPLIED SEDIMENTOLOGY[Internet]. 2018;5(10 ):43-63. Available from: https://sid.ir/paper/260580/en

    IEEE: Copy

    M. JANBAZ, H. MOHSENI, A.R. Piraee, B. YOUSEFI YEGANEH, and h. Seradeghi soofiani, “Depositional Environment of the Shahbazan Formation: a tail of evoloving ramp to shelf,” APPLIED SEDIMENTOLOGY, vol. 5, no. 10 , pp. 43–63, 2018, [Online]. Available: https://sid.ir/paper/260580/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