Late Neoproterozoic to Carboniferous genesis of A-type magmas in Avalonia of northern Nova Scotia: repeated partial melting of anhydrous lower crust in contrasting tectonic environments
Crossref DOI link: https://doi.org/10.1007/s00531-017-1512-7
Published Online: 2017-07-12
Published Print: 2018-03
Update policy: https://doi.org/10.1007/springer_crossmark_policy
Murphy, J. Brendan
Shellnutt, J. Gregory
Collins, William J.
Funding for this research was provided by:
Natural Sciences and Engineering Research Council of Canada
License valid from 2017-07-12