{"type":"Feature","properties":{"id":7489,"name":"Protomylonites of the Ferriere-Molli\u00e8res shear zone","description":"

Coarse grained protomylonitic gneiss (fig. 2a) with deformed leucosomes of K-feldspar, plagioclase and quartz in a medium grained biotite and sillimanite matrix with sometimes white mica. The amount of matrix is variable from a maximum of nearly 50% to a minimum of 30% – 40%. S-C fabric and asimmetric and stretched leucosomes are recognizable (fig. 2a), All the kinematic indicators point to a top-to-the SE sense of shear (fig. 2b).<\/p>\n

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