The occurrence of compositional and microtextural relies within metamorphic
rocks can provide useful information on the pressure-temperature history o
f the host rock. The grain-size of these microstructures, such as coronitic
reaction microtextures, is mostly too fine to be detected by optical micro
scopy, Therefore, a more detailed analytical approach is needed. In this pa
per multiple electron beam techniques including the acquisition of X-ray mu
lti-element maps, micro and nano-analysis performed by SEM/EDS and TEM/STEM
-EDX systems were applied to a specific petrological problem related to met
amorphism. Fine-grained decompressional reaction microtextures of an eclogi
tic sample (Mt. Rosa Nappe, Western Alps) are described and discussed.