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Information Journal Paper

Title

STUDY OF AMPHIBOLITES IN NORTH OF CHAH ZARD (EAST OF JANDAQ, NORTH-EAST OF ISFAHAN PROVINCE)

Pages

  121-132

Abstract

 In north of Chah Zard farm, Jandaq metamorphic complex contains schising and marble underlay the amphibolites. Amphibolites are metamorphosed basalts of JANDAQ OPHIOLITE. and JANDAQ METAMORPHIC ROCKS are metasedimentary cover of Jandaq metaophiolite. Ampbibolites contain hornblende, plagioclase, garnet, alkali feldspar (orthoclase), magnetite. biotite. muscovite, sphene and quartz. These rocks present very good lineation and foliation. By metamorphic differentiation. mafic and felsic minerals are seperated in some locations. Mineralogical studies. Hornblende barometry, and hornblende - plagioclase thermometry, conclude the metamorphism of these rocks under upper part of amphibolite facies (7.10 to 9.91 Kbars and 619 to 650°C). Presence of actinolite, epidote and calcite in amphibolites demonstrates a retrograde metamorphism under green schist facies.

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  • Cite

    APA: Copy

    TORABI, GH.. (2007). STUDY OF AMPHIBOLITES IN NORTH OF CHAH ZARD (EAST OF JANDAQ, NORTH-EAST OF ISFAHAN PROVINCE). RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", 27(1), 121-132. SID. https://sid.ir/paper/56002/en

    Vancouver: Copy

    TORABI GH.. STUDY OF AMPHIBOLITES IN NORTH OF CHAH ZARD (EAST OF JANDAQ, NORTH-EAST OF ISFAHAN PROVINCE). RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE"[Internet]. 2007;27(1):121-132. Available from: https://sid.ir/paper/56002/en

    IEEE: Copy

    GH. TORABI, “STUDY OF AMPHIBOLITES IN NORTH OF CHAH ZARD (EAST OF JANDAQ, NORTH-EAST OF ISFAHAN PROVINCE),” RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", vol. 27, no. 1, pp. 121–132, 2007, [Online]. Available: https://sid.ir/paper/56002/en

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