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:

860
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 STUDY OF YOUNG BASALTS IN EAST AZERBAIJAN (NORTHWEST OF IRAN)

Pages

  109-126

Abstract

 The young basalts in EAST AZERBAIJAN are placed in West Alborz – Azerbaijan zone. Volcanic activities have extended from the Pliocene to the Quaternary by eruption from fracture systems and faults. Rocks under study are olivine-basalt and trachybasalts. The main minerals are olivine, pyroxene, plagioclase set in glassy or microcrystalline matrix and olivine are present as phenocryst. The textures in the studied rocks are mainly hyaloporphyric, hyalomicrolitic and porphyritic. Trace elements and rare earth elements on spider diagrams have high LREE/HREE ratio. Rare earth elements on diagram display negative slope indicating alkaline nature for the basalts under study. As it may be observed, on tectonic diagrams, the Marand basalts are placed on Island Arc basalt (IAB) field, whereas the Ahar, Heris, Kalaibar and Miyaneh basalts are classified as Ocean Island Basalts (OIB) and finally the basalts of Sohrol area are plotted on continental rift Basalt (CRB) field. The Marand and Sohrol basalts were likely originated from lithospheric - astenospheric mantle with 2 to 5 % partial melting whereas, the Ahar, Heris and Kalaibar basalts having same source experienced 1-2% partial melting rate and the Miyaneh basalts possibly produced from lithospheric mantle with 10-20% partial melting rate pointing to shallow depth of mantle and the higher rate of melting. Based on tectonic setting diagrams, all the rocks studied are plotted in post collisional environments.

Cites

  • No record.
  • References

  • No record.
  • Cite

    APA: Copy

    AMEL, NASIR, & AKBARZADEH LALEH, MOUSA. (2017). GEOCHEMICAL STUDY OF YOUNG BASALTS IN EAST AZERBAIJAN (NORTHWEST OF IRAN). PETROLOGY, 7(28 ), 109-126. SID. https://sid.ir/paper/197063/en

    Vancouver: Copy

    AMEL NASIR, AKBARZADEH LALEH MOUSA. GEOCHEMICAL STUDY OF YOUNG BASALTS IN EAST AZERBAIJAN (NORTHWEST OF IRAN). PETROLOGY[Internet]. 2017;7(28 ):109-126. Available from: https://sid.ir/paper/197063/en

    IEEE: Copy

    NASIR AMEL, and MOUSA AKBARZADEH LALEH, “GEOCHEMICAL STUDY OF YOUNG BASALTS IN EAST AZERBAIJAN (NORTHWEST OF IRAN),” PETROLOGY, vol. 7, no. 28 , pp. 109–126, 2017, [Online]. Available: https://sid.ir/paper/197063/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