Tectonomagmatic characteristics of ophiolitic gabbroids from south Orzuieh (south of Baft, Kerman) ophiolite complex: insights from clinopyroxene chemistry

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Payghambari s.

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Journal: Iranian Journal of Crystallography and Mineralogy Year:2018 | Volume:26 | Issue:2 Page(s): 301-314

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Title

Tectonomagmatic characteristics of ophiolitic gabbroids from south Orzuieh (south of Baft, Kerman) ophiolite complex: insights from clinopyroxene chemistry

Author(s)

Payghambari s. | Issue Writer Certificate

Keywords

TectonomagmaticQ1

mineral chemistryQ1

clinopyroxeneQ2

layered ultramafic and maficQ1

ophioliteQ2

OrzuiehQ1

Abstract

Mafic and ultramafic layered rocks located in south of Orzuieh (Baft, Kerman province), consist of plagioclase bearing ultramafic rocks (including olivine, orthopyroxene, clinopyroxene and plagioclase), olivine gabbros (including plagioclase, olivine, orthopyroxene and clinopyroxene) and gabbronorites (including plagioclase, orthopyroxene and clinopyroxene and amphibole) and constitute the mafic parts of the Orzuieh colored mé lange complex. mineral chemistry of clinopyroxene show diopside end-member which have Mg# ranging from 0. 75 to 0. 88. According to geothermobarometric calculations, temperatures change from 783 to 975º C and pressure conditions vary from 1. 4 to 3. 6 kbar. Tectono-magmatic considerations show that these clinopyroxenes have been crystallized from tholeiitic to bonintic magmas which have already formed in an arc environment. Therefore, it could be considered that Orzuieh layered ultramafic and mafic rock series are some parts of ophiolitic complexes which occurred in a subduction setting.

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APA: Copy

Payghambari, s.. (2018). Tectonomagmatic characteristics of ophiolitic gabbroids from south Orzuieh (south of Baft, Kerman) ophiolite complex: insights from clinopyroxene chemistry. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 26(2 ), 301-314. SID. https://sid.ir/paper/389585/en

Vancouver: Copy

Payghambari s.. Tectonomagmatic characteristics of ophiolitic gabbroids from south Orzuieh (south of Baft, Kerman) ophiolite complex: insights from clinopyroxene chemistry. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2018;26(2 ):301-314. Available from: https://sid.ir/paper/389585/en

IEEE: Copy

s. Payghambari, “Tectonomagmatic characteristics of ophiolitic gabbroids from south Orzuieh (south of Baft, Kerman) ophiolite complex: insights from clinopyroxene chemistry,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 26, no. 2 , pp. 301–314, 2018, [Online]. Available: https://sid.ir/paper/389585/en

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