Stähle, V., Altherr, R., Trieloff, M., & Varychev, A. (2017). Majoritic garnet grains within shock-induced melt veins in amphibolites from the Ries impact crater suggest ultrahigh crystallization pressures between 18 and 9 GPa. Contributions to mineralogy and petrology, 172(10), . https://doi.org/10.1007/s00410-017-1404-7
Chicago-Zitierstil (17. Ausg.)Stähle, Volker, Rainer Altherr, Mario Trieloff, und Alexander Varychev. "Majoritic Garnet Grains Within Shock-induced Melt Veins in Amphibolites from the Ries Impact Crater Suggest Ultrahigh Crystallization Pressures Between 18 and 9 GPa." Contributions to Mineralogy and Petrology 172, no. 10 (2017). https://doi.org/10.1007/s00410-017-1404-7.
MLA-Zitierstil (9. Ausg.)Stähle, Volker, et al. "Majoritic Garnet Grains Within Shock-induced Melt Veins in Amphibolites from the Ries Impact Crater Suggest Ultrahigh Crystallization Pressures Between 18 and 9 GPa." Contributions to Mineralogy and Petrology, vol. 172, no. 10, 2017, https://doi.org/10.1007/s00410-017-1404-7.