MINERALOGY OF RODINGITES IN DEHSHIR-SURK OPHIOLITES

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NOGHREHEIAN M.; MAKIZADEH M.A.; SHERAFAT SH.; ASAD ELAHI P.

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Journal: RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE" Year:2006 | Volume:23 | Issue:1 Page(s): 79-103

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Title

MINERALOGY OF RODINGITES IN DEHSHIR-SURK OPHIOLITES

Author(s)

NOGHREHEIAN M. | MAKIZADEH M.A. | SHERAFAT SH. | ASAD ELAHI P. | Issue Writer Certificate

Keywords

OPHIOLITEQ3

RODINGITEQ3

CENTRAL IRANQ3

Abstract

Gabbroie dykes hostes in serpentinite of Dehshir-surk OPHIOLITEs have undergone hydrothermal alteration, well known as serpentinization. Serpentnization of primary minerals (Pyroxene, olivine) introuduces Ca+2 to hydrothermal fluids. These Ca-rich fluids are responsible for rodingitization of Gabbro dykes introuded in serpentinite basement.There are two distinct serpentinitization stages: dynamic and static. and it is concluded the rodingitization is a polygenic processse. The rare mineral pectolite [Na Ca2 Si3 O8 (OH)] is formed due to Na-metasomatism in the latest stage of hydrothermal processes.

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APA: Copy

NOGHREHEIAN, M., MAKIZADEH, M.A., SHERAFAT, SH., & ASAD ELAHI, P.. (2006). MINERALOGY OF RODINGITES IN DEHSHIR-SURK OPHIOLITES. RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", 23(1), 79-103. SID. https://sid.ir/paper/55956/en

Vancouver: Copy

NOGHREHEIAN M., MAKIZADEH M.A., SHERAFAT SH., ASAD ELAHI P.. MINERALOGY OF RODINGITES IN DEHSHIR-SURK OPHIOLITES. RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE"[Internet]. 2006;23(1):79-103. Available from: https://sid.ir/paper/55956/en

IEEE: Copy

M. NOGHREHEIAN, M.A. MAKIZADEH, SH. SHERAFAT, and P. ASAD ELAHI, “MINERALOGY OF RODINGITES IN DEHSHIR-SURK OPHIOLITES,” RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", vol. 23, no. 1, pp. 79–103, 2006, [Online]. Available: https://sid.ir/paper/55956/en

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