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Information Journal Paper

Title

RODINGITIZATION OF IRANIAN BASIC ROCKS: A NEW INTERPRETATION

Pages

  155-160

Abstract

 Mineral paragenesis of rodingitized basic rocks of Iranian ophiolites are presented and metasomatic reactions between Ca+2 bearing aqueous fluids issued during serpentinization of host ultramafic rock – with magmatic minerals of basic rocks leading to present paragenesis of rodingites are discussed. It is concluded that Ca+2 rich aqueous fluid in equilibrium with serpentinite has high Ca+2 chemical potential to react with magmatic minerals of basic dykes resulting in lowering the free energy of system, appearance of a new mineral paragenesis and total or partial conversion of basic dykes to rodingites. A feedback mechanism is proposed to account for inter-relationship of serpentinization and rodingitization.

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  • Cite

    APA: Copy

    SABZEHEI, M.. (2002). RODINGITIZATION OF IRANIAN BASIC ROCKS: A NEW INTERPRETATION. JOURNAL OF SCIENCES ISLAMIC REPUBLIC OF IRAN, 13(2), 155-160. SID. https://sid.ir/paper/368623/en

    Vancouver: Copy

    SABZEHEI M.. RODINGITIZATION OF IRANIAN BASIC ROCKS: A NEW INTERPRETATION. JOURNAL OF SCIENCES ISLAMIC REPUBLIC OF IRAN[Internet]. 2002;13(2):155-160. Available from: https://sid.ir/paper/368623/en

    IEEE: Copy

    M. SABZEHEI, “RODINGITIZATION OF IRANIAN BASIC ROCKS: A NEW INTERPRETATION,” JOURNAL OF SCIENCES ISLAMIC REPUBLIC OF IRAN, vol. 13, no. 2, pp. 155–160, 2002, [Online]. Available: https://sid.ir/paper/368623/en

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