M
Maurizio Mazzucchelli
Researcher at University of Modena and Reggio Emilia
Publications - 88
Citations - 2517
Maurizio Mazzucchelli is an academic researcher from University of Modena and Reggio Emilia. The author has contributed to research in topics: Mafic & Mantle (geology). The author has an hindex of 29, co-authored 84 publications receiving 2286 citations. Previous affiliations of Maurizio Mazzucchelli include University of Ferrara & Max Planck Society.
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Isotopic evidence from the Ivrea Zone for a hybrid lower crust formed by magmatic underplating
H. Voshage,A. W. Hofmann,Maurizio Mazzucchelli,Giorgio Rivalenti,Silvano Sinigoi,Ingrid Raczek,G. Demarchi +6 more
TL;DR: The large mafic complex overlying mantle peridotites in the Ivrea Zone of northern Italy originated by underplating of mantle-derived magma onto the base of continental crust as discussed by the authors.
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The Finero phlogopite-peridotite massif: an example of subduction-related metasomatism
TL;DR: In this article, the authors proposed a model where melts derived from an eclogite-facies slab infiltrate the overhanging harzburgitic mantle wedge and, because of the special thermal structure of subduction zones, become heated to the temperature of the peridotite.
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Metasomatism and Melting in Carbonated Peridotite Xenoliths from the Mantle Wedge: The Gobernador Gregores Case (Southern Patagonia)
Angela Laurora,Maurizio Mazzucchelli,Giorgio Rivalenti,Riccardo Vannucci,Alberto Zanetti,Maria Adelaide Barbieri,Carlos Alberto Cingolani +6 more
TL;DR: Laurora et al. as discussed by the authors presented an analysis of the relationship between the authorship of the authors and the authors of the paper, which is based on the Dipartamento Di Scienze Della Terra, Universita Di Modena e Reggio Emilia, Modena ; Italia
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Chemical evolution of a large mafic intrusion in the lower crust, Ivrea‐Verbano Zone, northern Italy
Silvano Sinigoi,James E. Quick,Diane Clemens-Knott,Adriano Mayer,Gabbriella Demarchi,Maurizio Mazzucchelli,L. Negrini,Giorgio Rivalenti +7 more
TL;DR: In this article, the contaminant is also shown to have been enriched in Ba with respect to Rb and K. The results of this study can be explained by melting of granulite-facies paragneiss, which had previously been depleted in K and Rb by an earlier melting event.
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Origin of LREE-depleted amphiboles in the subcontinental mantle
Riccardo Vannucci,Giovanni B. Piccardo,Giorgio Rivalenti,Alberto Zanetti,Elisabetta Rampone,Luisa Ottolini,Roberta Oberti,Maurizio Mazzucchelli,P. Bottazzi +8 more
TL;DR: In this article, anon-microprobe analyses of interstitial kaersutite and Ti-pargasite grains from orogenic peridotites and lherzolite xenoliths reveal that LREE-depleted amphiboles are common in the subcontinental mantle samples.