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Information Journal Paper

Title

VEIN HYDROTHERMAL METAMORPHISM OF JANDAQ OPHIOLITIC GABBROS (NE OF ISFAHAN PROVINCE)

Pages

  83-100

Abstract

JANDAQ OPHIOLITE suites are covered by metamorphic rocks that are marbles and schists. This old ophiolitic association has passed different phases of serpentinization and METAMORPHISM. In this rock association, gabbroic dikes cross cut the SERPENTINIZED MANTLE PERIDOTITES. Joints and cracks of brittle gabbroic dikes are filled by veins that are light in color. These veins are formed after METAMORPHISM and serpentinization. These coarse grain rocks are free from deformation and foliation, and are formed by calcite, prehnite, epidote, clinopyroxene and chlorite. The most important mineralogical characteristic of these veins is existence and considerable amount of calcite, that is the evidence of high f CO2 in minerals bearing fluid. Vein enclosing gabbros, are metamorphosed in amphibolite facies (2.7 to 9 kbar pressure and 630 to 750 of C temperature), and then pass through a retrograde METAMORPHISM in green schist facies.

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    Cite

    APA: Copy

    TORABI, GH.. (2008). VEIN HYDROTHERMAL METAMORPHISM OF JANDAQ OPHIOLITIC GABBROS (NE OF ISFAHAN PROVINCE). RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", 30(1 (GEOLOGY)), 83-100. SID. https://sid.ir/paper/56015/en

    Vancouver: Copy

    TORABI GH.. VEIN HYDROTHERMAL METAMORPHISM OF JANDAQ OPHIOLITIC GABBROS (NE OF ISFAHAN PROVINCE). RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE"[Internet]. 2008;30(1 (GEOLOGY)):83-100. Available from: https://sid.ir/paper/56015/en

    IEEE: Copy

    GH. TORABI, “VEIN HYDROTHERMAL METAMORPHISM OF JANDAQ OPHIOLITIC GABBROS (NE OF ISFAHAN PROVINCE),” RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", vol. 30, no. 1 (GEOLOGY), pp. 83–100, 2008, [Online]. Available: https://sid.ir/paper/56015/en

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