Abstract
Generally speaking, the structure of Albanides is divided in two large structural regions — inner Albanides and outer Albanides. Each of these regions manifests peculiar geological, tectonic and metallogenic characteristics. In the geological structuring of Albanides participates the old sediment of the Palaeozoic with a limited spreading, developing mainly in the eastern parts. The sediment of Mesozoic, mainly composed of carbonates, spreading to the south-western, central, and northern parts of Albania, has a greater development.
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© 2003 Springer Science+Business Media Dordrecht
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Demi, G., Myftiu, G., Themeli, G., Testard, J. (2003). Sustainable Development and Systems for Management of Mining Sector in Albania. In: Tvalchrelidze, A.G., Morizot, G. (eds) Mineral Resource Base of the Southern Caucasus and Systems for its Management in the XXI Century. NATO Science Series, vol 17. Springer, Dordrecht. https://doi.org/10.1007/978-94-010-0084-0_6
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DOI: https://doi.org/10.1007/978-94-010-0084-0_6
Publisher Name: Springer, Dordrecht
Print ISBN: 978-1-4020-1124-5
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