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The Skaergaard trough layering: sedimentation in a convecting magma chamber
The upper parts of the floor cumulates of the Skaergaard Intrusion, East Greenland, contain abundant features known as troughs. The troughs are gently plunging synformal structures comprising stacks of crescentic modally graded layers with a sharply defined mafic base that grades upward into plagioc...
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| Publicado en: | Contrib Mineral Petrol |
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| Autores principales: | , , , |
| Formato: | Artigo |
| Lenguaje: | Inglês |
| Publicado: |
Springer Berlin Heidelberg
2018
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| Materias: | |
| Acceso en línea: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6560677/ https://ncbi.nlm.nih.gov/pubmed/31258174 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1007/s00410-018-1466-1 |
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