Is the slab component in arc magmas produced by fluid-induced eclogitisation of subducted lower oceanic crust?.

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John, T., Scherer, E. E., Haase, K. and Schenk, V. (2004) Is the slab component in arc magmas produced by fluid-induced eclogitisation of subducted lower oceanic crust?. Geochimica Et Cosmochimica Acta, 68 (11). A601-A601.

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Document Type: Article
Research affiliation: Kiel University
Date Deposited: 24 Jan 2012 05:45
Last Modified: 09 Oct 2012 03:56
URI: https://oceanrep.geomar.de/id/eprint/16138

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