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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...

Ausführliche Beschreibung

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Bibliographische Detailangaben
Veröffentlicht in:Contrib Mineral Petrol
Hauptverfasser: Vukmanovic, Z., Holness, M. B., Monks, K., Andersen, J. C. Ø.
Format: Artigo
Sprache:Inglês
Veröffentlicht: Springer Berlin Heidelberg 2018
Schlagworte:
Online Zugang: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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