C
Costanza Bonadiman
Researcher at University of Ferrara
Publications - 70
Citations - 1862
Costanza Bonadiman is an academic researcher from University of Ferrara. The author has contributed to research in topics: Metasomatism & Mantle (geology). The author has an hindex of 19, co-authored 67 publications receiving 1641 citations.
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Carbonatite Metasomatism of the Oceanic Upper Mantle: Evidence from Clinopyroxenes and Glasses in Ultramafic Xenoliths of Grande Comore, Indian Ocean
TL;DR: Petrological and geochemical data for a suite of brought down in a subducting slab at a former convergent plate ultramafic xenoliths (lherzolites and wehrlites) from La Grille margin is presented in this article.
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Amphiboles from suprasubduction and intraplate lithospheric mantle
Massimo Coltorti,Costanza Bonadiman,Barbara Faccini,Michel Grégoire,Suzanne Y. O'Reilly,William Powell +5 more
TL;DR: In this article, geochemical features of amphiboles, mainly from mantle xenoliths, were investigated for a number of intraplate and suprasubduction localities, with the aim of fingerprinting the metasomatic signatures for the two different geological settings.
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Amphibole genesis via metasomatic reaction with clinopyroxene in mantle xenoliths from Victoria Land, Antarctica
Massimo Coltorti,Luigi Beccaluva,Costanza Bonadiman,Barbara Faccini,Theodoros Ntaflos,Franca Siena +5 more
TL;DR: Petrographic and major and trace element geochemical features of clinopyroxene, amphibole and glass from composite xenoliths from Mt. Melbourne and Mt. Overlord (Victoria Land, Antarctica) were investigated.
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Coexisting anorogenic and subduction-related metasomatism in mantle xenoliths from the Betic Cordillera (southern Spain)
TL;DR: In this paper, the authors show that peridotites in the spinel-to-plagioclase stability field of the Betic Cordillera of southern Spain can be attributed to at least two metasomatizing agents with distinct chemical and isotopic compositions.
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Glasses in mantle xenoliths as geochemical indicators of metasomatic agents
TL;DR: An extensive comparison between world-wide occurrences of mantle glasses in both continental and oceanic settings is presented in this article, where several localities were chosen on the basis of the available major (and trace) element data, coupled with a clear identification of the nature of the metasomatizing agents.