Majoritic garnet grains within shock-induced melt veins in amphibolites from the Ries impact crater suggest ultrahigh crystallization pressures between 18 and 9 GPa
Crossref DOI link: https://doi.org/10.1007/s00410-017-1404-7
Published Online: 2017-10-14
Published Print: 2017-10
Update policy: https://doi.org/10.1007/springer_crossmark_policy
Stähle, Volker
Altherr, Rainer
Nasdala, Lutz
Trieloff, Mario
Varychev, Alexander
License valid from 2017-10-01