Title |
Fig. 5. The dependence of the composition of schreiberzite on the temperature of its formation during crystallization from melts and subsolidus reactions. Schreiberzite (1) - rims on non-metallic inclusions and xenomorphic grains along the boundaries of the metal. Schreiberzite (2) - idiomorphic elongated-prismatic crystals of schreibersite in the Widmannstetten metal structure. Schreiberzite (3) isometric crystals in a recrystallized Widmanshetten metal structure. Schreiberzite (4) is a matrix in the regions of local melting. |
Submission |
Crystallisation of the metal in iie irons and possible meteorite analog |
Type |
Исследовательские инструменты |
Date |
2019-08-29 |
Digital Object Identifier |
https://doi.org/10.31857/S0016-7525648826-836-14254 |