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which according to its similar lithologies and
tectonothermal evolution can be correlated with
the Agualada Unit of the Órdenes Complex. The
lowest structural level of the Cabo Ortegal Com-
plex is occupied by a thick serpentinite mélange
restricted to the advancing front of the allochtho-
nous complexes, the Somozas Mélange. This is an
exotic unit for which no equivalent units have
3. GEOLOGICAL FRAMEWORK
Fig. 5.
Geological map and representative cross sections of the Malpica–Tui Complex. Based on Díez Fernández (2011).