Fe3+ reduction during biotite melting in graphitic metapelites: another origin of CO2 in granulites. (Articolo in rivista)

Type

• Prodotto della ricerca (Classe)
• Articolo in rivista (Classe)

Label

• Fe3+ reduction during biotite melting in graphitic metapelites: another origin of CO2 in granulites. (Articolo in rivista) (literal)

Anno

• 2005-01-01T00:00:00+01:00 (literal)

Alternative label

• Cesare B., Meli S., Nodari L., Russo U. (2005)
  Fe3+ reduction during biotite melting in graphitic metapelites: another origin of CO2 in granulites.
  in Contributions to mineralogy and petrology
  (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori

• Cesare B., Meli S., Nodari L., Russo U. (literal)

Pagina inizio

• 129 (literal)

Pagina fine

• 140 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume

• 149 (literal)

Rivista

• Contributions to mineralogy and petrology (Rivista)

Note

• ISI Web of Science (WOS) (literal)

Titolo

• Fe3+ reduction during biotite melting in graphitic metapelites: another origin of CO2 in granulites. (literal)

Abstract

• The Fe3+/Fetot of all Fe-bearing minerals has been analysed by Mössbauer spectroscopy in a suite of biotite-rich to biotite-free graphitic metapelite xenoliths, proxies of an amphibolite-granulite transition through progressive biotite melting. Biotite contains 9 to 16% Fe3+/Fetot, whereas garnet, cordierite and ilmenite are virtually Fe3+ -free (0–1% Fe3+/Fetot) in all samples, regardless of biotite presence. Under relatively reducing conditions (graphite-bearing assemblages), biotite is the only carrier of Fe3+ during high-temperature metamorphism; therefore, its disappearance by melting represents an important event of iron reduction during granulite formation, because haplogranitic melts usually incorporate small amounts of ferric iron. Iron reduction is accompanied by the oxidation of carbon and the production of CO2. (literal)

Prodotto di

• Geodinamica ed evoluzione della litosfera continentale (TA.P04.015.003) (Modulo)
• Istituto di geoscienze e georisorse (IGG) (Istituto)

Autore CNR

• LUCA NODARI (Unità di personale interno)
• BERNARDO CESARE (Persona)

Incoming links:

Prodotto

• Istituto di geoscienze e georisorse (IGG) (Istituto)
• Geodinamica ed evoluzione della litosfera continentale (TA.P04.015.003) (Modulo)

Autore CNR di

• BERNARDO CESARE (Persona)
• LUCA NODARI (Unità di personale interno)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#rivistaDi

• Contributions to mineralogy and petrology (Rivista)