TECTONITE PERIDOTITES STUDIES OF KHOY OPHIOLITE

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KHALILI KHADIJEH; PAHLEVANINJAD REZA

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

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Journal: PETROLOGY Year:2010 | Volume:1 | Issue:2 Page(s): 31-42

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Information Journal Paper

Title

TECTONITE PERIDOTITES STUDIES OF KHOY OPHIOLITE

Author(s)

KHALILI KHADIJEH | PAHLEVANINJAD REZA | Issue Writer Certificate

Keywords

OPHIOLITEQ2

TECTONIC PERIDOTITESQ3

KHOYQ2

REEQ2

Abstract

The KHOY OPHIOLITE with Precambrian basement rock is located in north western of Iran.The tectonite peridotites are most formed by clinopyroxene harzburgites. These harzburgites characterized by protogranular, porphyroclastic and transformation textures, and composed of olivine (with kink band), orthopyroxene (with wavy extinction and exsolution clinopyroxene), spinel (like Holly – Leaf and shaped) and less than 10% of clinopyroxene. Two stages of alteration occur in these rocks, including static and dynamic. These peridotites are partial melting residual of spinel lherzolites.The KHOY taconite periodontitis show the U-form pattern in the REEs. These patterns are probably related to the partial melting procedures and the process following the partial melting such as influence of felsic magmas after emplacement of OPHIOLITEs.

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APA: Copy

KHALILI, KHADIJEH, & PAHLEVANINJAD, REZA. (2010). TECTONITE PERIDOTITES STUDIES OF KHOY OPHIOLITE. PETROLOGY, 1(2), 31-42. SID. https://sid.ir/paper/196895/en

Vancouver: Copy

KHALILI KHADIJEH, PAHLEVANINJAD REZA. TECTONITE PERIDOTITES STUDIES OF KHOY OPHIOLITE. PETROLOGY[Internet]. 2010;1(2):31-42. Available from: https://sid.ir/paper/196895/en

IEEE: Copy

KHADIJEH KHALILI, and REZA PAHLEVANINJAD, “TECTONITE PERIDOTITES STUDIES OF KHOY OPHIOLITE,” PETROLOGY, vol. 1, no. 2, pp. 31–42, 2010, [Online]. Available: https://sid.ir/paper/196895/en

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