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Magmatic evidence for carbonate metasomatism in the lithospheric mantle underneath the Ohre (Eger) Rift

Brandl, Philipp; Genske, Felix S.; Beier, C; Haase, Karsten M; Sprung, Peter; Krumm, Stefan H.


Magmas erupted in intracontinental rifts typically form from melting of variable proportions of asthenospheric or lithospheric mantle sources and ascend through thick continental lithosphere. This ascent of magma is accompanied by differentiation and assimilation processes. Understanding the composition of rift-related intracontinental volcanism is important, particularly in densely populated active rift zones such as the Ohře (Eger) Rift in Central Europe. We have sampled and analysed...[Show more]

CollectionsANU Research Publications
Date published: 2015
Type: Journal article
Source: Journal of Petrology
DOI: 10.1093/petrology/egv052


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