New evidence for upper Permian crustal growth below Eifel, Germany, from mafic granulite xenoliths
<p>Granulite xenoliths from the Quaternary West Eifel Volcanic Field in Germany record evidence of magmatism in the lower crust at the end of the Permian. The xenoliths sampled two distinct bodies: an older intrusion (ca. 264 Myr old) that contains clinopyroxene with flat, chondrite-normalised...
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2021-04-01
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| Series: | European Journal of Mineralogy |
| Online Access: | https://ejm.copernicus.org/articles/33/233/2021/ejm-33-233-2021.pdf |