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:

737
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, PETROGENESIS AND TECTONIC SETTING OF THE SARCHESHMEH EOCENE MAFIC LAVA FLOWS, SOUTHWEST OF RAFSANJAN

Pages

  209-220

Abstract

 The EOCENE mafic lava flows of SARCHESHMEHare cropped out in the southwest of Rafsanjan area at the central part of the Urmia – Dokhtar magmatic belt. The rocks are BASALT, BASALTic ANDESITE and ANDESITE in composition and consist of clinopyroxene+plagioclase ± olivine ± hornblende phenocrysts. The geochemical characteristics show CALC-ALKALINE nature for the lavas that are formed in an ACTIVE CONTINENTAL MARGIN tectonic environment. Low amounts of MgO, Cr and Ni in the SARCHESHMEH EOCENE BASALTic lavas points to the role of evolution in their parental magma. The MORB normalized multi-element patterns of the lava flows show enrichment in LILE (e.g. Sr, K, Rb and Ba) and depletion in HFSE (e.g. Ta, Nb and Ti). The Chondrite-normalized REE patterns show moderate enrichments in LREE with (La/Yb)n<3 for all samples. The geochemical features such as (La/Yb)n<2, the Yb contents and also using petrological diagrams based on trace and rare earth element ratios (e.g. Th/Y, Nb/Y, Ta/Yb, Ce/Yb) indicate that the SARCHESHMEH EOCENE BASALTic lavas were generated from a metasomatized lithospheric mantle source at the spinel stability depth.

Cites

  • No record.
  • References

  • No record.
  • Cite

    APA: Copy

    HOSSEINI, S.Z.. (2016). GEOCHEMISTRY, PETROGENESIS AND TECTONIC SETTING OF THE SARCHESHMEH EOCENE MAFIC LAVA FLOWS, SOUTHWEST OF RAFSANJAN. GEOSCIENCES, 25(100), 209-220. SID. https://sid.ir/paper/31692/en

    Vancouver: Copy

    HOSSEINI S.Z.. GEOCHEMISTRY, PETROGENESIS AND TECTONIC SETTING OF THE SARCHESHMEH EOCENE MAFIC LAVA FLOWS, SOUTHWEST OF RAFSANJAN. GEOSCIENCES[Internet]. 2016;25(100):209-220. Available from: https://sid.ir/paper/31692/en

    IEEE: Copy

    S.Z. HOSSEINI, “GEOCHEMISTRY, PETROGENESIS AND TECTONIC SETTING OF THE SARCHESHMEH EOCENE MAFIC LAVA FLOWS, SOUTHWEST OF RAFSANJAN,” GEOSCIENCES, vol. 25, no. 100, pp. 209–220, 2016, [Online]. Available: https://sid.ir/paper/31692/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