The arcuate pattern of the main Caledonian cleavage and associated fold axial plane traces in North Wales is due partly to NW‐SE compression with tectonic transport to the southeast against the concealed crop of the Tan y grisiau Microgranite. Low‐angle cleavage close to the microgranite is shown to be a local variant of the regional cleavage formed during the main deformation and not an earlier phase as previously supposed. Transcurrent movements along several major fault systems are also related to compression around the microgranite and the Harlech Dome block.
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Campbell et al. (1985) studied this question.
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