| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 8910731 | Geochimica et Cosmochimica Acta | 2018 | 25 Pages |
Abstract
The high Csâ¯+â¯Rbâ¯Â±â¯B concentrations of melt and fluid inclusions in sulfur-rich magmatic apatite (0.3-1.4â¯wt% SO3) suggest a pegmatitic environment for the exsolution of the fluids. The similar element/K ratios of liquid-rich inclusions in the late-stage pyrite-quartz veins to the fluid inclusions in the sulfur-rich apatite suggest that the late-stage fluids were also likely derived from highly evolved melt fractions in felsic magmas during the solidification of the magma chamber.
Keywords
Related Topics
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Geochemistry and Petrology
Authors
Jia Chang, Jian-Wei Li, Andreas Audétat,