Contaminating melt flow in magmatic peridotites from the lower continental crust (Rocca d'Argimonia sequence, Ivrea–Verbano Zone)
<p>The lower continental crust section of the Ivrea–Verbano Zone (Italian Alps) was intruded by a <span class="inline-formula">∼</span> 8 km thick gabbroic–dioritic body (Ivrea Mafic Complex) in the Upper Carboniferous–Lower Permian, in conjunction w...
Main Authors: | , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2020-11-01
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Series: | European Journal of Mineralogy |
Online Access: | https://ejm.copernicus.org/articles/32/587/2020/ejm-32-587-2020.pdf |