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Figure 1. A polished pyrope megablast section with partial talc + chlorite
alteration along fractures and rims. The red square shows an example of a
millimeter-sized fracture-free garnet area selected for this study with zircon
and coesite crystalline inclusions exhibiting strain-induced birefringent haloes
in the surrounding host have been found.
Campomenosi et al. https://doi.org/10.2138/am-2018-6700CCBY