Crystals reveal magma convection and melt transport in dyke-fed eruptions
The processes and ranges of intensive variables that control magma transport and dyke propagation through the crust are poorly understood. Here we show that textural and compositional data of olivine crystals (Mg/Fe, Ni and P) from the tephra of the first months of Paricutin volcano monogenetic erup...
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| Main Authors: | , , , , |
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| 格式: | Article |
| 語言: | English |
| 出版: |
2021
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| 在線閱讀: | https://hdl.handle.net/10356/146071 |
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