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Figure S1: Mineral chemistry and melt evolution of the mantle wedge peridotites in the Late Cretaceous Zagros Belt ophiolites (Iran): clues for the subduction initiation-induced forearc magmatism
العنوان: | Figure S1: Mineral chemistry and melt evolution of the mantle wedge peridotites in the Late Cretaceous Zagros Belt ophiolites (Iran): clues for the subduction initiation-induced forearc magmatism |
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المؤلفون: | Ghasem Ghorbani, Hadi Shafaii Moghadam, Yildirim Dilek, Shoji Arai, Mohamed Z. Khedr |
سنة النشر: | 2024 |
المجموعة: | Geological Society of London: Figshare |
مصطلحات موضوعية: | Geology, mantle wedge peridotites, iran ): clues, induced forearc magmatism, large olivine crystals, kermanshah isotropic gabbros, neyriz olivine gabbros, grained olivine gabbros, neyriz harzburgites, grained cr, serpentinized olivine, olivine porphyroclasts, subduction initiation, scattered images, mineral chemistry, melt evolution, following features, figure s1, abad harzburgites, abad dunites |
الوصف: | Figure S1. Back-scattered images of Zagros mantle rocks reveal the following features: A. Orthopyroxene, clinopyroxene, and olivine porphyroclasts with small spinel crystals within Kermanshah lherzolites. B. Olivine and dark brown spinel crystals embedded in large clinopyroxene crystals within Kermanshah lherzolite cumulates. C. Large olivine crystals, clinopyroxene, and plagioclase present in coarse-grained olivine gabbros from Kermanshah. D. Olivine, clinopyroxene, and plagioclase in Kermanshah isotropic gabbros. E. Olivine, anhedral orthopyroxene and tiny clinopyroxene in Neyriz harzburgites. F. Olivine, clinopyroxene and plagioclase in Neyriz olivine gabbros. G- Serpentinized olivine and anhedral orthopyroxene in Haji-Abad harzburgites. H- Serpentinized olivine and medium to coarse-grained Cr-spinels in Haji-Abad dunites. |
نوع الوثيقة: | still image |
اللغة: | unknown |
Relation: | https://figshare.com/articles/figure/Figure_S1_Mineral_chemistry_and_melt_evolution_of_the_mantle_wedge_peridotites_in_the_Late_Cretaceous_Zagros_Belt_ophiolites_Iran_clues_for_the_subduction_initiation-induced_forearc_magmatism/25296112 |
DOI: | 10.6084/m9.figshare.25296112.v1 |
الاتاحة: | https://doi.org/10.6084/m9.figshare.25296112.v1 https://figshare.com/articles/figure/Figure_S1_Mineral_chemistry_and_melt_evolution_of_the_mantle_wedge_peridotites_in_the_Late_Cretaceous_Zagros_Belt_ophiolites_Iran_clues_for_the_subduction_initiation-induced_forearc_magmatism/25296112 |
Rights: | CC BY 4.0 |
رقم الانضمام: | edsbas.9D843021 |
قاعدة البيانات: | BASE |
DOI: | 10.6084/m9.figshare.25296112.v1 |
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