Bernardo Cesare
University of Padua
87 Papers
514 Citations
Bernardo Cesare is an academic researcher from University of Padua. The author has contributed to research in topics: Melt inclusions & Anatexis. The author has an hindex of 33, co-authored 82 publications. Previous affiliations of Bernardo Cesare include University of Los Andes.
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Papers
C‐O‐H‐S fluid composition and oxygen fugacity in graphitic metapelites
TL;DR: In this article, the authors considered graphitic metamorphic systems in which the dominant fluid source is dehydration, e.g. graphite-saturated fluids produced entirely by dehydration, and the variance of the dehydration process is not increased in comparison with that in nongraphitic systems.
304
Melted Rocks under the Microscope: Microstructures and Their Interpretation
TL;DR: The evolution of these structures during prograde melting and later, later, retrograde cooling can be understood using concepts derived from experimental simulation and materials science as mentioned in this paper, which can be used to understand the former presence of melt in rocks which have undergone cooling and exhumation over millions of years.
196
Occurrence and Origin of Andalusite in Peraluminous Felsic Igneous Rocks
D. B. Clarke,Michael J. Dorais,B. Barbarin,Daniel S. Barker,Bernardo Cesare,Geoffrey L. Clarke,M. El Baghdadi,Saskia Erdmann,Hans-Jürgen Förster,Martha Leticia Gaeta,B. Gottesmann,Rebecca Anne Jamieson,Daniel J. Kontak,Friedrich Koller,CL Gomes,David London,George B. Morgan,Ljpf Neves,Drm Pattison,Ajsc Pereira,Michel Pichavant,Carlos W. Rapela,Axel D. Renno,Simon Richards,Malcolm P. Roberts,A. Rottura,J. Saavedra,Alcides N. Sial,Alejandro J. Toselli,JM Ugidos,Pavel Uher,Carlos Villaseca,Dario Visonà,Donna L. Whitney,Ben J. Williamson,HH Woodard +35 more
TL;DR: In this paper, the authors examined 108 samples of andalusite-bearing felsic rocks from more than 40 localities world-wide and found that the majority of them show no textural or chemical evidence suggesting a magmatic origin.
Crustal anatexis and melt extraction during deformation in the restitic xenoliths at El Joyazo (se spain)
TL;DR: The dacite of El Joyazo contains abundant metapelitic xenoliths as discussed by the authors, which can be divided into two main types: garnet-biotite-sillimanite and spinel-cordierite.
Hydrogen deficiency in Ti-rich biotite from anatectic metapelites (El Joyazo, SE Spain): Crystal-chemical aspects and implications for high-temperature petrogenesis
TL;DR: In this article, the presence of Ti in the octahedral site of biotite is consistent with the Ti-oxy exchange, whereas Ti-Tschermak or Ti-vacancy substitutions play a very minor role.