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Trace-element distribution coefficients for pyroxenes, plagioclase, and olivine in evolved tholeiites from the 1955 eruption of Kilauea Volcano, Hawaii, and petrogenesis of differentiated rift-zone lavas

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Authors

Norman, Marc
Garcia, Michael
Pietruszka, Aaron

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Mineralogical Society of America

Abstract

Reliable values for mineral-melt trace-element distribution coefficients (D) are essential for constructing realistic models of magma evolution based on trace elements. We have determined D-values for an extensive set of compatible and incompatible trace

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American Mineralogist

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