Experimentally induced volumetric re-equilibration of plagioclase-hosted melt inclusions
The application of melt inclusions (MI) to infer magmatic processes assumes the MI have remained as constant mass, constant volume systems since the time of trapping. Understanding the effects of both compositional and volumetric re-equilibration is key for the interpretation of MI data. Although th...
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Main Authors: | , , , , |
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格式: | Article |
語言: | English |
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2021
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在線閱讀: | https://hdl.handle.net/10356/146830 |
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