MINERALOGY OF DIFFERENT PHASES OF RODINGITE FORMATION IN DIKES OF ANARAK UPPER PROTEROZOIC OPHIOLITE (NE OF ISFAHAN PROVINCE, IRAN)

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TORABI GH.A.; SABZEHEI M.; ARAI S.; ABMED H.A.; EMAMI M.H.; MOHAJEL MOHAMMAD

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Journal: Iranian Journal of Crystallography and Mineralogy Year:2004 | Volume:12 | Issue:1 Page(s): 77-92

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Title

MINERALOGY OF DIFFERENT PHASES OF RODINGITE FORMATION IN DIKES OF ANARAK UPPER PROTEROZOIC OPHIOLITE (NE OF ISFAHAN PROVINCE, IRAN)

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Keywords

MINERALOGYQ4

GEOCHEMISTRYQ2

OPHIOLITEQ2

SERPENTINIZED MANTLE PERIDOTITEQ4

DIKESQ3

INTRUSIVESQ3

RODINGITESQ4

Abstract

In north of Anarak area, in the upper Proterozoic OPHIOLITE, exist Massive and Vein type RODINGITES. Vein type RODINGITES have fonned in two phases. Massive or Static RODINGITES have fonned during oceanic crust spreading and OPHIOLITE fonnation, and Vein type or Dynamic RODINGITES have fonned during Anarak OPHIOLITE emplacement and tectonic activities. Abundance order of minerals in massive RODINGITES is Garnet (Chromian- Andradite), Idocrase, Chlorite, Diopside, Prehnite and Epidote (decreasing). In the first phase of vein type RODINGITES, the abundance order of minerals is Diopside, Chlorite, Idocrase, and Garnet (Ti-Andradite), and in the second phase is Diopside, Chlorite and Garnet (Andradite). Petrography and geochemical study of minerals show that, during the fonnation of massive type RODINGITES, the activity of Calcium, Iron, and Chromium ions in fluids, and during the fonnation of first phase of vein type RODINGITES, the activity of Calcium, Silicon, Magnesium, Aluminum, Titanium, and OH- ions in fluids, have been increased. GEOCHEMISTRY of second phase of vein type RODINGITES is similar to first phase, but because of absence of Idocrase, and low Titanium in Andradite structure, the activity of Iron, Titanium, and Aluminum ions, is lower than first phase. Generally the diversity of minerals in massive type RODINGITES is more than vein type RODINGITES.

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APA: Copy

TORABI, GH.A., SABZEHEI, M., ARAI, S., ABMED, H.A., EMAMI, M.H., & MOHAJEL, MOHAMMAD. (2004). MINERALOGY OF DIFFERENT PHASES OF RODINGITE FORMATION IN DIKES OF ANARAK UPPER PROTEROZOIC OPHIOLITE (NE OF ISFAHAN PROVINCE, IRAN). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 12(1), 77-92. SID. https://sid.ir/paper/3813/en

Vancouver: Copy

TORABI GH.A., SABZEHEI M., ARAI S., ABMED H.A., EMAMI M.H., MOHAJEL MOHAMMAD. MINERALOGY OF DIFFERENT PHASES OF RODINGITE FORMATION IN DIKES OF ANARAK UPPER PROTEROZOIC OPHIOLITE (NE OF ISFAHAN PROVINCE, IRAN). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2004;12(1):77-92. Available from: https://sid.ir/paper/3813/en

IEEE: Copy

GH.A. TORABI, M. SABZEHEI, S. ARAI, H.A. ABMED, M.H. EMAMI, and MOHAMMAD MOHAJEL, “MINERALOGY OF DIFFERENT PHASES OF RODINGITE FORMATION IN DIKES OF ANARAK UPPER PROTEROZOIC OPHIOLITE (NE OF ISFAHAN PROVINCE, IRAN),” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 12, no. 1, pp. 77–92, 2004, [Online]. Available: https://sid.ir/paper/3813/en

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