Fig. 5

A D1 syntectonic garnet from the sample RM-02-04 in the greesnschist facies zone of the Miyar Valley. B, C Staurolite—garnet bearing sample collected in the staurolite zone. The geometry of the internal foliation S2 preserved in the staurolite porphyrolast indicate a static growth of the staurolite on the S2 foliation after the phse of deformation D3. D Relative chronology between the deformation phases and related structures and crystallization of the index metamorphic minerals for samples form the greenschist (left) and staurolite zone (right). Terra-Wasserburg diagram for U-Pb analyses of monazite for the staurolite bearing sample constraining the growth of staurlite at ca. 41 Ma (illustration modified from Robyr and Lanari, 2020)