Article ID Journal Published Year Pages File Type
9451153 Chemie der Erde - Geochemistry 2005 12 Pages PDF
Abstract
The presence of fluid inclusions in chromite aggregates hosted in orthopyroxenite dikes, in combination with the trace element contents in chromite concentrates and the mineralogical composition of the dikes may indicate that an aqueous phase separated from the magma.
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Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
Preview
Fluid inclusions in chromite from a pyroxenite dike of the Pindos ophiolite complex
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