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:

3,308
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

MINERALOGY, PETROGRAPHY AND PETROGENESIS OF SAHAND VOLCANIC SUITE, NORTHWEST IRAN

Pages

  83-102

Abstract

SAHAND volcanic rocks, with Plio-Quaternery age, is located southeast Tabriz in the northwest part of CENTRAL IRAN. These rocks are mainly composed of pyroclastics (tuff and ignimberite) and lava flows (rhyolite, rhyodacite, dacite and andesite) that unconformably cover the Miocene sedimentary formations. The major constituent minerals include plagioclase and hornblende which are surrounded by a matrix of fine grain and glassy. Their textures are porphyritic. Heterogenous mineralogy, field and textural evidences such as sieve texture in plagioclase, resorption rims in crystals, oscillatory zoning in plagioclase, high normative quartz and rounded enclaves suggest that the primary magma undergone magmatic evolution including fractional crystallization, fractionation, contamination and magma mixing during ascending. There are mineralogical as well as geochemical evidences that AFC-type processes were involved in the evolution of the SAHAND volcanic rocks. The chemistry of the felsic- intermediate volcanic rocks indicates that the parent magmas are medium-K calc-alkaline and metaluminous in nature. The volcanic rocks display highly fractionated REE patterns, with no negative Eu anomaly. Their geotectonic environment is post-collision and continental margin arcs.

Cites

  • No record.
  • References

  • No record.
  • Cite

    APA: Copy

    PIRMOHAMMADI, F., AMERI, A., JAHANGIRI, A., MOJTAHEDI, M., CHEN, CH., & KESKIN, M.. (2011). MINERALOGY, PETROGRAPHY AND PETROGENESIS OF SAHAND VOLCANIC SUITE, NORTHWEST IRAN. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 19(1), 83-102. SID. https://sid.ir/paper/4027/en

    Vancouver: Copy

    PIRMOHAMMADI F., AMERI A., JAHANGIRI A., MOJTAHEDI M., CHEN CH., KESKIN M.. MINERALOGY, PETROGRAPHY AND PETROGENESIS OF SAHAND VOLCANIC SUITE, NORTHWEST IRAN. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2011;19(1):83-102. Available from: https://sid.ir/paper/4027/en

    IEEE: Copy

    F. PIRMOHAMMADI, A. AMERI, A. JAHANGIRI, M. MOJTAHEDI, CH. CHEN, and M. KESKIN, “MINERALOGY, PETROGRAPHY AND PETROGENESIS OF SAHAND VOLCANIC SUITE, NORTHWEST IRAN,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 19, no. 1, pp. 83–102, 2011, [Online]. Available: https://sid.ir/paper/4027/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