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:

950
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

MINERAL CHEMISTRY AND PETROGENESIS OF CALC-ALKALINE LAMPROPHYRIC DIKES AT SUNGUN AND HAFTCHESHME MINES (ALBORZ- AZARBAIJAN ZONE, IRAN)

Pages

  47-60

Abstract

 Sungun and HAFTCHESHME mines are located in the Arasbaran volcano-plutonic complex at the North West of Azarbaijan province. Lamprophyric dikes of SUNGUN with ages younger than Oligo-Miocene contain biotite, plagioclase and pyroxene with porphyritic texture and are classified as calc-alkaline and KERSANTITE. They are intruded into the SUNGUN quartz - monzonite. Lamprophyric dikes of HAFTCHESHME with ages younger than Oligo-Miocene include minerals such asbiotite, alkali feldspar and pyroxene. The main textures are microlithic porphyry and flow texture. These CALC-ALKALINE LAMPROPHYREs are classified as MINETTE, intruding the HAFTCHESHME quartz - diorite. The behavior of trace elements studied by the means of spider diagrams show low enrichment of LREE relative to MREE and HREE. Investigations on geochemical characteristics of the studied lamprophyres show that the lamprophyric rocks are of calc-alkaline type, formed in a magmatic arc tectonic setting. These lamprophyres are generated from low degree partial melting of a garnet lherzolite source.

Cites

  • No record.
  • References

  • No record.
  • Cite

    APA: Copy

    GHAREHCHAHI, Z., MOAYYED, M., AHMADIYAN, J., & MURATA, M.. (2017). MINERAL CHEMISTRY AND PETROGENESIS OF CALC-ALKALINE LAMPROPHYRIC DIKES AT SUNGUN AND HAFTCHESHME MINES (ALBORZ- AZARBAIJAN ZONE, IRAN). GEOSCIENCES, 27(105 ), 47-60. SID. https://sid.ir/paper/32280/en

    Vancouver: Copy

    GHAREHCHAHI Z., MOAYYED M., AHMADIYAN J., MURATA M.. MINERAL CHEMISTRY AND PETROGENESIS OF CALC-ALKALINE LAMPROPHYRIC DIKES AT SUNGUN AND HAFTCHESHME MINES (ALBORZ- AZARBAIJAN ZONE, IRAN). GEOSCIENCES[Internet]. 2017;27(105 ):47-60. Available from: https://sid.ir/paper/32280/en

    IEEE: Copy

    Z. GHAREHCHAHI, M. MOAYYED, J. AHMADIYAN, and M. MURATA, “MINERAL CHEMISTRY AND PETROGENESIS OF CALC-ALKALINE LAMPROPHYRIC DIKES AT SUNGUN AND HAFTCHESHME MINES (ALBORZ- AZARBAIJAN ZONE, IRAN),” GEOSCIENCES, vol. 27, no. 105 , pp. 47–60, 2017, [Online]. Available: https://sid.ir/paper/32280/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