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The geology of the complex, poorly exposed and highly deformed and metamorphosed rocks of the Sudetes of SW Poland has long been controversial.
‘Marble’ is a general term for any kind of limestone or other carbonate rock that has been metamorphosed .
Two facies of regionally metamorphosed rocks that may be of either original sedimentary or igneous derivation are characterized by epidote.
These rocks were metamorphosed during the Grampian Orogeny.
This rock unit consists chiefly of Silurian shale and sandstone that have been metamorphosed to high-grade schist and migmatite.
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