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Title

Petrography, geochemistry and petrogenesis of Qale Gabra granitoid Rocks (south-west of Jiroft-Kerman province)

Pages

  257-270

Abstract

 The Qale Gabra granitoid rocks is located in Kerman province, south-west of Jiroft, Sanandaj-Sirjan belt. This plutonic rocks has upper Jurassic age and intruded to the lower Jurassic Sedimentary rocks. Based on Field geology, mineralogy and geochemistary studies, the lithology composition of the area consists of granodiorite, monzogranite, syenogranite, granite rich in quartz and diorite-gabbro. geochemical diagrams, shows a vast magmatic differentiation during crystalization. According to genetical classification it belongs to I type and Magnetite series. Tectonic setting discrimination diagrams shows relation of this mass with VAG and based on other geochemical data it has a Meta Alumine-PerAlumine and Calc Alkaline with low postassium affinity. LREE and LILE enrichment and Nb, Ti depletion may be has been occurred for a crustal contamination in a subduction zone. As it located on Urmia-Dokhtar magmatic belt is seems that, This area is a product of subduction of Neothetis under central Iranian continental crust.

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    APA: Copy

    KHALILI MOBARHAN, SH., & Khosravi Mashizi, S.. (2019). Petrography, geochemistry and petrogenesis of Qale Gabra granitoid Rocks (south-west of Jiroft-Kerman province). GEOSCIENCES, 29(113 ), 257-270. SID. https://sid.ir/paper/31394/en

    Vancouver: Copy

    KHALILI MOBARHAN SH., Khosravi Mashizi S.. Petrography, geochemistry and petrogenesis of Qale Gabra granitoid Rocks (south-west of Jiroft-Kerman province). GEOSCIENCES[Internet]. 2019;29(113 ):257-270. Available from: https://sid.ir/paper/31394/en

    IEEE: Copy

    SH. KHALILI MOBARHAN, and S. Khosravi Mashizi, “Petrography, geochemistry and petrogenesis of Qale Gabra granitoid Rocks (south-west of Jiroft-Kerman province),” GEOSCIENCES, vol. 29, no. 113 , pp. 257–270, 2019, [Online]. Available: https://sid.ir/paper/31394/en

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