Fig. 4
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Outcrop of mafic-ultramafic rocks. (a) Sigmoid-shaped pyroxenite boudins in migmatitic pyroxenite. (b) Sigmoid-shaped amphibolite boudins in migmatitic amphibolite. (c) Ovoid-shaped metahornblendite enclave rimmed by amphibolite bands concordant to the Smgm foliation. (d) Amphibolite enclaves hosted in mylonitic diorite. (e) Fn+2 isoclinal folded granitic vein in metahornblendite. (f) Fn+3 disharmonic folds of amphibolite showing sinistral motion within mylonitic granodiorite. (g) δ-type marker showing a dextral kinematic movement. (h) S0/n compositional banding developed in the banded garnet amphibolite. The illustrations were observed on subhorizontal planes.
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