REMARKS ON THE KARSTIFICATION IN THE WIDER AREA OF THE UPPER MESSINIA CLOSED HYDROGEOLOGICAL BASIN (SW PELOPONNESUS, GREECE)

Autor: E. Spyridonos, I. Mariolakos

Publikováno v: Δελτίο της Ελληνικής Γεωλογικής Εταιρείας; Τόμ. 43 Αρ. 4 (2010): 12o Διεθνές Συνέδριο της Ελληνικής Γεωλογικής Εταιρίας; 1785-1791
Bulletin of the Geological Society of Greece; Vol. 43 No. 4 (2010): 12th International Conference of the G.S.G.; 1785-1791

The Upper Messinia Basin is part of the Kalamata - Kyparissia graben structure, defined by two fault zones, one of E-W direction to the north and one of N-S direction to the east. The Tripolis and the Pindos alpidic units build up the basement of the

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::27b89afce2367928d505365589d06ed2
https://doi.org/10.12681/bgsg.11364