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:

1,017
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:

3

Information Journal Paper

Title

GEOCHEMISTRY OF AYRAKAN INTRUSION, APLITIC DIKE AND ENCLAVES (NE OF ISFAHAN PROVINCE)

Pages

  13-32

Abstract

 The area of study is in the North of khur and North-East of Arusan-e-kur-e-Gaz, which in geology divisions is in Central Iran. In petrographic study intrusive body, APLITIC DIKEs and ENCLAVEs are alkali granite. Minerals of alkali granites are K-feldspar (orthoclase and microcline), plagioclase (albite and oligoclase), quartz with undoluse straight extinction, biotite, muscovite, zircon and apatite. Chlorite is created by biotite alteration. Intrusive body has foliation in many parts that look like auegen gneiss in the first view. But investigations show that this intrusive mass is mylonitized.Geochemical investigation shows the nature of calc alkalin, peraluminous and S-type nature of understudy granitoids. Thus samples of studying area located in syncollision region. The temperature given by two feldspars thermometry, that is lower than temperature of igneous environment, present the sub-solidus changes of feldspars composition. Ti in biotite thermometry result 632-661oC for biotites of intrusive body, APLITIC DIKEs and ENCLAVEs. The obtained temperatures reveal the igneous temperatures of biotite crystallization. In addition, chlorites of alkali granites display a temperature around 188oC. This temperature indicates the biotite alteration temperature.

Cites

References

  • No record.
  • Cite

    APA: Copy

    BAHARZADEH, H., TORABI, GH., AHMADIAN, J., & EBRAHIMIYAN, Z.. (2008). GEOCHEMISTRY OF AYRAKAN INTRUSION, APLITIC DIKE AND ENCLAVES (NE OF ISFAHAN PROVINCE). RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", 32(3 (GEOLOGY)), 13-32. SID. https://sid.ir/paper/55820/en

    Vancouver: Copy

    BAHARZADEH H., TORABI GH., AHMADIAN J., EBRAHIMIYAN Z.. GEOCHEMISTRY OF AYRAKAN INTRUSION, APLITIC DIKE AND ENCLAVES (NE OF ISFAHAN PROVINCE). RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE"[Internet]. 2008;32(3 (GEOLOGY)):13-32. Available from: https://sid.ir/paper/55820/en

    IEEE: Copy

    H. BAHARZADEH, GH. TORABI, J. AHMADIAN, and Z. EBRAHIMIYAN, “GEOCHEMISTRY OF AYRAKAN INTRUSION, APLITIC DIKE AND ENCLAVES (NE OF ISFAHAN PROVINCE),” RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", vol. 32, no. 3 (GEOLOGY), pp. 13–32, 2008, [Online]. Available: https://sid.ir/paper/55820/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