Brittle and ductile: The boudinage is primarily a brittle process, as portrayed by quartz-filled fractures (white), while the folding is ductile (although very low temperature, probably <300 C). What a beautiful area to study cleavage formation, folding, fracturing and boudinage!
See Reber et al. (Tectonoph. 2010, v 493, 187-195) and Marques (Tectonics 2010) for more information.
Chocolate boudinaged fold limb.
Axial planar cleavage in metasandstone.
Folded turbidites.
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