Reactive flow as dominant evolution process in the lowermost oceanic crust: evidence from olivine of the Pineto ophiolite (Corsica)
Crossref DOI link: https://doi.org/10.1007/s00410-015-1194-8
Published Online: 2015-10-12
Published Print: 2015-10
Update policy: https://doi.org/10.1007/springer_crossmark_policy
Sanfilippo, Alessio http://orcid.org/0000-0002-4112-3643
Tribuzio, Riccardo
Tiepolo, Massimo
Berno, Davide
Funding for this research was provided by:
Ministero dell’Istruzione, dell’Università e della Ricerca (20099SWLYC)
Text and Data Mining valid from 2015-10-01