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Mygdonia Basin is an active seismotectonic zone. Its regional geology is characterized by step-faulted metamorphosed Paleozoic and Mesozoic sediments partly intruded by igneous rocks. Two geothermal anomalies, heating groundwater to more than 40°C at 100 m below the surface, are tied to horst-like basement uplifts along deep-reaching faults. Inorganic carbon dissolved in thermal waters of the region...
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