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The thickness of the crystal mush on the floor of the Bushveld magma chamber
The thickness of the crystal mush on magma chamber floors can be constrained using the offset between the step-change in the median value of dihedral angles formed at the junctions between two grains of plagioclase and a grain of another phase (typically clinopyroxene, but also orthopyroxene and oli...
Uloženo v:
| Vydáno v: | Contrib Mineral Petrol |
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| Hlavní autoři: | , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Springer Berlin Heidelberg
2017
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6959381/ https://ncbi.nlm.nih.gov/pubmed/32009664 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1007/s00410-017-1423-4 |
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