Diopside and Magnetite Exsolutions in Olivine from Lower Cr Dunite in the Dongbo Ophiolite, Southern Tibet

Acta Geologica Sinica-english Edition(2015)

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摘要
Diopside and magnetite exsolutions occur as oriented intergrowths within olivine of the lower Cr # dunite in the Dongbo ophiolite,Tibet.The fresh lower Cr # dunite has a mineral assemblage of olivine,spinel and diopside.The Fo content of its olivine is 90–92,which is lower than that of the higher Cr # dunite lenses(Fo92-Fo94)without
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magnetite exsolutions,dongbo ophiolite,tibet,olivine
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