Bernardo Cesare - Selected Publications#


Cesare B., Campomenosi, N., Shribak, M. (2022) Polychromatic polarization: boosting the capabilities of the good old petrographic microscope. Geology, 50, 137–141.

Cesare B., Parisatto M., Mancini L., Peruzzo L., Franceschi M., Tacchetto T., Reddy S., Spiess R., Nestola F., Marone F. (2021) Mineral inclusions are not immutable: evidence of post-entrapment thermally-induced shape change of quartz in garnet. EPSL, 555, 116708.

Carvalho B. B., Bartoli O., Cesare B., Tacchetto T., Gianola O., Ferri F., Aradi L.E. and Szabó C. (2020) Primary fluid inclusions in granulitic garnet usually do not survive. EPSL., 536, 116170.

Bartoli O., Cesare, B. (2020) Nanorocks: a 10-year-old story. Rendiconti Lincei, 31, 249–257.

Tacchetto T., Bartoli O., Cesare B., Berkesi M., Aradi L.E., Dumond G., Szabó C. (2019) Multiphase inclusions in peritectic garnet from granulites of the Athabasca granulite terrane (Canada): evidence of carbon recycling during Neoarchean crustal anatexis. Chemical Geology, 508, 197-209

Cesare B., Nestola F., Johnson T., Mugnaioli E., Della Ventura G., Peruzzo L., Bartoli O., Viti C., Erickson T. (2019) Garnet, the archetypal cubic mineral, grows tetragonal. Scientific Reports 9, Article number: 14672.

Parisatto M., Turina A., Cruciani G., Mancini L., Peruzzo L., Cesare B. (2018) 3D distribution of primary melt inclusions in garnets by X-ray microtomography. American Mineralogist, 103, 911–926.

Cesare B., Acosta-Vigil A., Bartoli O., Ferrero S. (2015) What can we learn from melt inclusions in migmatites and granulites? Lithos, 239, 186-216.

Sawyer, E.W., Cesare, B. & Brown M. (Editors) When the continental crust melts. Elements, (vol. 7, August 2011).

Cesare B., Ferrero S., Salvioli-Mariani E., Pedron D. e Cavallo A. (2009) Nanogranite and glassy inclusions: the anatectic melt in migmatites and granulites. Geology, 37, 627-630.

Imprint Privacy policy « This page (revision-4) was last changed on Thursday, 1. June 2023, 17:48 by System
  • operated by