S
Sandro Conticelli
Researcher at University of Florence
Publications - 128
Citations - 5394
Sandro Conticelli is an academic researcher from University of Florence. The author has contributed to research in topics: Volcanic rock & Mafic. The author has an hindex of 40, co-authored 118 publications receiving 4826 citations. Previous affiliations of Sandro Conticelli include University of Basilicata & Kyoto University.
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Journal ArticleDOI
Analogue modelling of continental extension: a review focused on the relations between the patterns of deformation and the presence of magma
Giacomo Corti,Marco Bonini,Sandro Conticelli,Fabrizio Innocenti,Piero Manetti,Dimitrios Sokoutis +5 more
TL;DR: In terms of causative processes, continental rifting may be explained by both active or passive mechanisms, which also differ in the volume of magmatic products and in the rheological properties and stratification of the extending lithosphere as mentioned in this paper.
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Petrology and geochemistry of potassic and ultrapotassic volcanism in central Italy: petrogenesis and inferences on the evolution of the mantle sources
TL;DR: In this article, trace element, Sr isotopic and mineral chemical data are reported for mafic volcanic rocks (Mg-value ⩾ 65) from the northern-central sector of the potassic volcanic belt of Central Italy.
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Trace elements and Sr-Nd-Pb isotopes of K-rich, shoshonitic, and calc-alkaline magmatism of the Western Mediterranean Region: Genesis of ultrapotassic to calc-alkaline magmatic associations in a post-collisional geodynamic setting
Sandro Conticelli,Luisa Guarnieri,Alice Farinelli,Massimo Mattei,Riccardo Avanzinelli,Gianluca Bianchini,Elena Boari,Simone Tommasini,Massimo Tiepolo,Dejan Prelević,Giampiero Venturelli +10 more
TL;DR: In this article, high-MgO ultrapotassic rocks are found in four different areas of the Western Mediterranean basin associated in space and time with shoshonitic and calc-alkaline rocks.
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Mediterranean Tertiary lamproites derived from multiple source components in postcollisional geodynamics
TL;DR: In the Mediterranean area, lamproites are derived from melts with three components involved in their origin, characterized by contrasting geochemical features which appear in 206Pb/204Pb, 87Sr/86Sr, and 143Nd/144Nd space as discussed by the authors.
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Source contamination and mantle heterogeneity in the genesis of Italian potassic and ultrapotassic volcanic rocks: Sr–Nd–Pb isotope data from Roman Province and Southern Tuscany
TL;DR: In this article, the Tyrrhenian border of the Italian peninsula has been the site of intense magmatism from Pliocene to recent times, and a decrease of alkaline character in time and space (southward) is observed.