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Information Journal Paper

Title

PETROLOGY OF ROCKS IN CONTACT OF MANTLE PERIDOTITE AND GABBRO INTRUSIONS IN THE CENTRAL IRAN OPHIOLITES (JANDAQ, ANARAK, NAEIN AND ASHIN)

Pages

  1-22

Abstract

 By intrusion of gabbros in MANTLE PERIDOTITES of the CENTRAL IRAN OPHIOLITES, a chemical potential gradient established and new metasomatic rocks are formed in CONTACT ZONE. These rocks produced by this special type of contact metamorphism, are clinopyroxenite, olivine clinopyroxenite wehrlite, lherzolite plagioclase peridotite and troctolite, from mantle peridotite side to the gabbro side. The studied rocks are formed at the expense of peridotitic part of the CONTACT ZONE. The occurrence of these types of reactions in ophiolitic associations are required a careful sampling and attention should be focused on the interpretation of gabbroic, peridotitic and pyroxenitic rocks data.

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    Cite

    APA: Copy

    TORABI, GH.. (2008). PETROLOGY OF ROCKS IN CONTACT OF MANTLE PERIDOTITE AND GABBRO INTRUSIONS IN THE CENTRAL IRAN OPHIOLITES (JANDAQ, ANARAK, NAEIN AND ASHIN). RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", 29(3 (GEOLOGY)), 1-22. SID. https://sid.ir/paper/55915/en

    Vancouver: Copy

    TORABI GH.. PETROLOGY OF ROCKS IN CONTACT OF MANTLE PERIDOTITE AND GABBRO INTRUSIONS IN THE CENTRAL IRAN OPHIOLITES (JANDAQ, ANARAK, NAEIN AND ASHIN). RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE"[Internet]. 2008;29(3 (GEOLOGY)):1-22. Available from: https://sid.ir/paper/55915/en

    IEEE: Copy

    GH. TORABI, “PETROLOGY OF ROCKS IN CONTACT OF MANTLE PERIDOTITE AND GABBRO INTRUSIONS IN THE CENTRAL IRAN OPHIOLITES (JANDAQ, ANARAK, NAEIN AND ASHIN),” RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", vol. 29, no. 3 (GEOLOGY), pp. 1–22, 2008, [Online]. Available: https://sid.ir/paper/55915/en

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