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:

724
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

GEOCHEMISTRY AND PETROGENESIS OF KUH-SHAH GRANITOIDIC PLUTON (NE BAFT)

Pages

  182-193

Abstract

 Kuh- Shah granitoidic pluton is located in the NE part of 1:100000 geological map of BAFT. Lithological composition of this plutonincludes Alkali- feldspar granite, granite, granodiorite, quartzdiorite, diorite and gabbro. This pluton has been intruded in volcaniclastics of Eocene age. On the variation diagrams the trends of major and trace elements of studied samples indicate the continuity of lithological compositional range of this pluton and they have been from differentiation of a basic (basaltic) magma. From the genetic classification point of view the studied granitoidic pluton is from I type granite and it belongs to magnetite series. Based on the geochemical features Kuh-Shah granitoidic pluton is metaluminous with high and medium potassic calcalkaline nature. High amounts of LILE and low amount of HFSE on the spider diagrams show that the parental magma of these rockshave been enriched from trace elements and incompatible elements. Based on the tectonic setting discrimination diagrams, this pluton is belong to VAG type and therefore it has been resulted from subduction of neotethys oceanic crust beneath the central IRAN continental crust.

Cites

  • No record.
  • References

  • No record.
  • Cite

    APA: Copy

    SADEGHI, ZAHRA, MAHDIZADEH, H., & SADEGHIAN, MAHMOUD. (2008). GEOCHEMISTRY AND PETROGENESIS OF KUH-SHAH GRANITOIDIC PLUTON (NE BAFT). GEOSCIENCES, 17(66), 182-193. SID. https://sid.ir/paper/31814/en

    Vancouver: Copy

    SADEGHI ZAHRA, MAHDIZADEH H., SADEGHIAN MAHMOUD. GEOCHEMISTRY AND PETROGENESIS OF KUH-SHAH GRANITOIDIC PLUTON (NE BAFT). GEOSCIENCES[Internet]. 2008;17(66):182-193. Available from: https://sid.ir/paper/31814/en

    IEEE: Copy

    ZAHRA SADEGHI, H. MAHDIZADEH, and MAHMOUD SADEGHIAN, “GEOCHEMISTRY AND PETROGENESIS OF KUH-SHAH GRANITOIDIC PLUTON (NE BAFT),” GEOSCIENCES, vol. 17, no. 66, pp. 182–193, 2008, [Online]. Available: https://sid.ir/paper/31814/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