Zobrazeno 1 - 10
of 52
pro vyhledávání: '"Federico CASETTA"'
Peridotite xenoliths from kimberlites are useful tools for exploring the architecture and composition of the thick sub-cratonic lithosphere, and thus understanding the long-term evolution of the Earth’s mantle. However, the continuous infiltration
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::527365800bcc56746e9782178a027b3d
https://doi.org/10.5194/egusphere-egu23-12712
https://doi.org/10.5194/egusphere-egu23-12712
Autor:
Nicolò Nardini, Federico Casetta, Chiara Maria Petrone, Massimo Coltorti, Theodoros Ntaflos Ntaflos
The Southalpine tectonic domain hosts numerous magmatic manifestations related to the trachybasaltic to trachyandesitic magmatic event that shaped the area during the Ladinian age (Middle Triassic). The identification of systematic compositional zoni
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::67b560ca656d740eaba051fd675b2741
https://doi.org/10.5194/egusphere-egu23-14606
https://doi.org/10.5194/egusphere-egu23-14606
Autor:
Andrea Luca Rizzo, Federico Casetta, Barbara Faccini, Luca Faccincani, Andres Sandoval-Velasquez, Alessandro Aiuppa, Massimo Coltorti
The investigation of mantle-derived products coming from Sub Continental Lithospheric Mantle (SCLM) is crucial for understanding its geochemical features and evolution, the mantle-crust interaction, and the volatiles composition. In this respect, min
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d89e0d8e4627c0af653f44ad9caafe37
https://doi.org/10.5194/egusphere-egu23-15035
https://doi.org/10.5194/egusphere-egu23-15035
Autor:
Massimo Coltorti, Nicolò Nardini, Federico Casetta, Lorenzo Tavazzani, Stefano Peres, Theodoros Ntaflos, Elio Dellantonio
Due to the complex geodynamic framework and the excellent state of preservation of the stratigraphic relationships towards the host metamorphic and sedimentary rocks, the Permo-Triassic magmatic sequences of the Southern Alps (Italy) are intensely st
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ac7b4ac363cf47c8e5bae602d47c6b19
https://doi.org/10.5194/egusphere-egu23-16555
https://doi.org/10.5194/egusphere-egu23-16555
Integrating petrography and mineral chemistry data with the determination of volatiles concentration and isotopic fingerprint in fluid inclusions (FI) in ultramafic xenoliths is a novel approach which provides crucial information on the nature and ev
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5b0368eeea892f56d023b3db1399ec31
https://doi.org/10.5194/egusphere-egu23-16798
https://doi.org/10.5194/egusphere-egu23-16798
Autor:
Gabriele Lanzafame, Pier Paolo Giacomoni, Federico Casetta, Lucia Mancini, Gianluca Iezzi, Massimo Coltorti, Carmelo Ferlito
Publikováno v:
Journal of Petrology. 63
Understanding lava flow dynamics during major effusive events is of paramount importance in volcanic areas characterized by a high risk of lava invasion. Mount Etna volcano (Sicily, Italy) has a long history of eruptions characterized by the emplacem
Publikováno v:
Nature Geoscience. 14:697-703
Carbon in the upper mantle controls incipient melting of carbonated peridotite and so acts as a critical driver of plate tectonics. The carbon-rich melts that form control the rate of volatile outflux from the Earth’s interior, contributing to clim
Autor:
Beatrice Pelorosso, Federico Casetta, Costanza Bonadiman, Cristina Perinelli, Pier Paolo Giacomoni, Barbara Faccini, Massimo Coltorti
Publikováno v:
Geological Society, London, Memoirs. 56:57-82
A review of northern Victoria Land ultramafic xenoliths, collected and studied over more than 30 years, was carried out. More than 200 samples were gathered and characterized in a coherent and comparative manner, both for mantle-derived and cumulate
Publikováno v:
Acta Geochimica. 40:623-639
The present work deals with the mineralogy, geochemical behavior and uranium potentiality of the monzogranites of El Maghrbia area, which comprise G. El Maghrbia and G. El Eredyia and situated in the central Eastern Desert of Egypt. G. El-Erediya mon
Unravelling the processes taking place during the genesis of kimberlites, their ascent through the sub-cratonic mantle and their emplacement in the crust is challenging, as kimberlites are mixtures of mantle-derived and magmatic components, rarely pr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::974814a9ecc631dee48d60ad2e32964f
https://doi.org/10.5194/egusphere-egu22-9214
https://doi.org/10.5194/egusphere-egu22-9214