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Information Journal Paper

Title

STUDY OF SKARNS IN NORTH OF NAIN OPHIOLITIC MELANGE (ISFAHAN PROVINCE, IRAN)

Pages

  221-228

Abstract

 Metamorphic rocks of NAIN OPHIOLITIC MELANGE consist amphibolitic dikes, amphibolite, SKARN, banded meta-chert, and succession of schist and marble. SKARNs exist as a white layer between upper part of amphibolites and lower part of banded meta-cherts. Petrographical studies and geochemistry of minerals show that the major minerals of SKARNs are carbonate (calcite), clinopyroxene (salite), garnet (grossular-andradite), and wollastonite, and the accessory minerals are sphene and epidote. SKARNs have produced by metamorphism of carbonate part of banded cherts and limestone, by a granite intrusion. Hornblenede-Plagioclase geothermometer show amphibolites and amphibolitic dikes are produced in amphibolite facies. One of the most important results of this study is presentation of this matter that "The metamorphic rocks in this OPHIOLITIC MELANGE are not exotic blocks, and they have produced by metamorphismof oceanic crust and covering sedimentary rocks"

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  • Cite

    APA: Copy

    TORABI, GH., ARAEI, SH., SHIR DASHTZADEH, N., SHIRASAKA, M., JABARI, A.A.R., & TORABI, H.. (2006). STUDY OF SKARNS IN NORTH OF NAIN OPHIOLITIC MELANGE (ISFAHAN PROVINCE, IRAN). RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", 23(1), 221-228. SID. https://sid.ir/paper/404751/en

    Vancouver: Copy

    TORABI GH., ARAEI SH., SHIR DASHTZADEH N., SHIRASAKA M., JABARI A.A.R., TORABI H.. STUDY OF SKARNS IN NORTH OF NAIN OPHIOLITIC MELANGE (ISFAHAN PROVINCE, IRAN). RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE"[Internet]. 2006;23(1):221-228. Available from: https://sid.ir/paper/404751/en

    IEEE: Copy

    GH. TORABI, SH. ARAEI, N. SHIR DASHTZADEH, M. SHIRASAKA, A.A.R. JABARI, and H. TORABI, “STUDY OF SKARNS IN NORTH OF NAIN OPHIOLITIC MELANGE (ISFAHAN PROVINCE, IRAN),” RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", vol. 23, no. 1, pp. 221–228, 2006, [Online]. Available: https://sid.ir/paper/404751/en

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