Post-collisional alkaline magmatism as gateway for metal and sulfur enrichment of the continental lower crust

Volume: 223, Pages: 175 - 197
Published: Feb 1, 2018
Abstract
Mafic and ultramafic magmas that intrude into the lower crust can preserve evidence for metal and sulfur transfer from the lithospheric mantle into the lower continental crust. Here we focus on a series of ultramafic, alkaline pipes in the Ivrea Zone (NW Italy), which exposes deeply buried (6–11 kbar), migmatitic metasedimentary rocks intruded by voluminous basaltic magmas of the Mafic Complex, a major crustal underplating event precisely dated...
Paper Details
Title
Post-collisional alkaline magmatism as gateway for metal and sulfur enrichment of the continental lower crust
Published Date
Feb 1, 2018
Volume
223
Pages
175 - 197
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