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:

1,829
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:

1

Information Journal Paper

Title

PETROLOGY OF QUATERNARY BASALTS OF TABAS (EAST OF IRAN)

Pages

  26-39

Abstract

 In southeastern TABAS there is a 400 square kilometer area of Quaternary BASALTs, which is geologically located in Lut zone. According to petrographic studies and EMPA analysis, the textures of these rocks are generally porphyric and some times aphyric. The phenocrysts of these BASALTs are generally chrisolite, augite, and plagioclase (andesine to labradorite), which are embedded in a texture of plagioclase microlites and small blades of pyroxene. According to the diagrams of accumulative amount of alkaline against the amount of SiO2, the nature of the magma is alkaline to sub-alkaline. The reason for the sub-alkaline character of some of these rocks is that the alkaline magma has been contaminated with crust materials. One of the most important reasons for this is the reduction of niobium in rocks enriched with SiO2. The alkaline samples have normative nepheline and the sub-alkaline samples normative quartz. The studies of Nd and Sr isotopes have confirmed the crust contamination and also the source for early magma of BASALTs is the upper parts of mantle. Based on the field studies and tectono- magmatic diagrams, these BASALTs are of intercontinental type because of the activities of great fault of Nayband in Quaternary and separation in their cross point reaching the earth’s surface.

Cites

References

  • No record.
  • Cite

    APA: Copy

    HASHEMI, SEYED MOHAMMAD, EMAMI, MOHAMMAD HASHEM, VOSOUGHI ABEDINI, M., POURMOAFI, M., & GHORBANI, MOSTAFA. (2008). PETROLOGY OF QUATERNARY BASALTS OF TABAS (EAST OF IRAN). GEOSCIENCES, 17(68), 26-39. SID. https://sid.ir/paper/32393/en

    Vancouver: Copy

    HASHEMI SEYED MOHAMMAD, EMAMI MOHAMMAD HASHEM, VOSOUGHI ABEDINI M., POURMOAFI M., GHORBANI MOSTAFA. PETROLOGY OF QUATERNARY BASALTS OF TABAS (EAST OF IRAN). GEOSCIENCES[Internet]. 2008;17(68):26-39. Available from: https://sid.ir/paper/32393/en

    IEEE: Copy

    SEYED MOHAMMAD HASHEMI, MOHAMMAD HASHEM EMAMI, M. VOSOUGHI ABEDINI, M. POURMOAFI, and MOSTAFA GHORBANI, “PETROLOGY OF QUATERNARY BASALTS OF TABAS (EAST OF IRAN),” GEOSCIENCES, vol. 17, no. 68, pp. 26–39, 2008, [Online]. Available: https://sid.ir/paper/32393/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