Mantle fragmentation and incomplete core merging of colliding planetesimals as evidenced by pallasites
Nicolas P. Walte, Christopher M. Howard, Gregor J. Golabek Earth and Planetary Science LettersVolume 617, 1 September 2023, 118247 LINK “Main group pallasites were likely formed by the collision of their parent body with a…
Olivines in main-group pallasites: magma-ocean cumulates or partial melting residues?OPEN ACCESS
J.-A. Barrat, L. Ferrière Geochemical Perspectives Letters v16Published 21 January 2021 LINK (OPEN ACCESS)PDF (OPEN ACCESS) “Main-group pallasites (MGPs) are meteorites mainly composed of Fe-Ni metal and olivines, the latter being considered as one of…