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However, quarry outcrops of mainly white halitic mylonites display isoclinal folds that suggest a more impressive past.
These mylonites are microstructurally more homogeneous than other types, and consist of very finegrained calcite that displays an elongate grain shape fabric.
The hanging-wall mylonite consists of an interconnected muscovite and chlorite network within a quartz-rich matrix.
Fine-grained mylonite developed in the fault corridor may have favoured aseismic deformation in the Shin volcano area.
The formation and preservation of the peridotite mylonite in particular presents problems of interpretation.
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