Article ID Journal Published Year Pages File Type
6441038 Lithos 2011 20 Pages PDF
Abstract
► Andong Ultramafic Complex, Korea comprises peridotites, pyroxenites and lesser gabbros. ► Petrographic and chemical data indicate that mafic-ultramafic rocks are magmatic. ► Bulk rock and mineral chemistry data suggest formation in supra-subduction zone (SSZ)/arc environment. ► Peridotite bulk rock and spinel chemistry record evidence of extensive melt-rock interaction.
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Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
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Magmatic peridotites and pyroxenites, Andong Ultramafic Complex, Korea: Geochemical evidence for supra-subduction zone formation and extensive melt-rock interaction
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