Fine structure of the whiteschist sample (IMAGE)
Caption
One of the pink garnet grains (left image, embedded in a matrix of quartz, rutile and phengite) with SiO2 inclusions (quartz inclusions), from which cracks originate. Numerical models (right image) predicts the generation of garnet failure.
Credit
Thibaut Duretz, Goethe University Frankfurt
Usage Restrictions
To be used only when reporting on Cindy et al. Nature Communications (2023) https://doi.org/10.1038/s41467-023-41310-w
License
Original content