The geological structure of mainland Greece (pre-Alpine and Alpine system-
structure) is examined, the discrimination between Internal and External Geotectonic
zones – units. The major Greek metallogenic provinces are examined, focused on the
most important Greek mineral resources and deposits (e.g. chromite, bauxite, Ni-
laterites, precious, base and strategic metals, industrial minerals, fossil fuels). The
correlation of Greek metallogenic provinces with the geologic, geodynamic and
geotectonic evolution of Greece is presented, and how these processes led to the
creation of the Greek mineral resources and deposits. Furthermore, insights in future
research and exploration for mineral deposits based on the geology and geologic
evolution of Greece are also discussed. Finally, the basic concepts of special
techniques related to ore deposit research (e.g. stable and radiogenic isotopes) are
taught, as well as the contemporary analytical techniques facilitating mineral
exploration.
- Teacher: Σταύρος Τριανταφυλλίδης
ECTS : 4
Language : el
Learning Outcomes : Upon successful completion of the course, the student will be able to: • Recognize which potential types of deposits and consequently useful components can be found in Greece. • Recognize the type of deposit and correlate the geological evolution of Greece with metallogeny. • Recognize the particular geological, tectonic, and geodynamic characteristics of an area and identify the potential types of deposits that can be found. • Recognize potential types of deposits in areas where no research has been carried out, such as the Central and Southern Aegean, to determine Greece s mineral potential.