Leucogranite dykes (K-feldspar + quartz + tourmaline ± white mica) cross cutting E-dipping schist and quartzite with migmatitic structures (paragenesis: biotite + andalusite + cordierite + K-feldspar + plagioclase + quartz). Photo credits: Samuele Papeschi References: Papeschi, S., Musumeci, G., Massonne, H.J., Bartoli, O., & Cesare, B. (2019). Partial melting and strain localization in metapelites…
Leucogranite dykes (K-feldspar + quartz + tourmaline ± white mica) cross cutting E-dipping schist and quartzite with migmatitic structures (paragenesis: biotite + andalusite + cordierite + K-feldspar + plagioclase + quartz).
Photo credits: Samuele Papeschi
References:
Papeschi, S., Musumeci, G., Massonne, H.J., Bartoli, O., & Cesare, B. (2019). Partial melting and strain localization in metapelites at very low-pressure conditions: The northern Apennines magmatic arc on the Island of Elba, Italy. Lithos, 350, 105230. https://doi.org/10.1016/j.lithos.2019.105230