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

Journal Paper

Paper Information

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:

863
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

GEOCHEMICAL AND SEDIMENTOLOGY CHARACTERISTICS OF DARIYAN FORMATION IN FARS AREA, CASE STUDY: KUH-E SIYAH AND SABZPOUSHAN WELL#1

Pages

  3-14

Abstract

 In this investigation DARIYAN FORMATION with the age of Lower Cretaceous (Aptian-Albian) were studied for GEOCHEMICAL and SEDIMENTOLOGY characteristics in the surface section at Kuh-e Siyah Anticline and subsurface section Sabzpushan well number 1. Based on petrographical studies 12 MICROFACIES identified which are belonging to 5 facies belt, such as: intertidal, lagoon, shoal, shallow open marine and deep open marine. The observed facies patterns indicated a carbonate ramp depositional environment. Important DIAGENETIC PROCESSES were observed in DARIYAN FORMATION including cementation, physical and chemical compaction and replacement processes such as pyritization and silicification. Prosities in these sections are secondary, including vuggy, fracture and channel types. Major and minor elements and carbon and oxygen isotopes studies are indicated that aragonite was original carbonate mineralogy for this Formation. The plots of elemental values also are illustrated that mainly burial DIAGENETIC PROCESSES have been affected this formation in semi-close to semi-open system. A temperature calculation based on the heaviest oxygen isotope value indicates that the very early, shallow burial temperature was around 28.5°C during Dariyan carbonate deposition.

Cites

  • No record.
  • References

  • No record.
  • Cite

    APA: Copy

    ADABI, M.H., ABBASI, R., & GHALAVAND, H.. (2011). GEOCHEMICAL AND SEDIMENTOLOGY CHARACTERISTICS OF DARIYAN FORMATION IN FARS AREA, CASE STUDY: KUH-E SIYAH AND SABZPOUSHAN WELL#1. GEOSCIENCES, 21(81), 3-14. SID. https://sid.ir/paper/32023/en

    Vancouver: Copy

    ADABI M.H., ABBASI R., GHALAVAND H.. GEOCHEMICAL AND SEDIMENTOLOGY CHARACTERISTICS OF DARIYAN FORMATION IN FARS AREA, CASE STUDY: KUH-E SIYAH AND SABZPOUSHAN WELL#1. GEOSCIENCES[Internet]. 2011;21(81):3-14. Available from: https://sid.ir/paper/32023/en

    IEEE: Copy

    M.H. ADABI, R. ABBASI, and H. GHALAVAND, “GEOCHEMICAL AND SEDIMENTOLOGY CHARACTERISTICS OF DARIYAN FORMATION IN FARS AREA, CASE STUDY: KUH-E SIYAH AND SABZPOUSHAN WELL#1,” GEOSCIENCES, vol. 21, no. 81, pp. 3–14, 2011, [Online]. Available: https://sid.ir/paper/32023/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