REMARKS ON THE KARSTIFICATION IN THE WIDER AREA OF THE UPPER MESSINIA CLOSED HYDROGEOLOGICAL BASIN (SW PELOPONNESUS, GREECE)
Περίληψη
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 region, and are covered by post-alpidic Pleistocene and quaternary deposits. The Basin is a closed hydrogeological system. In the upper cretaceous Pindos limestones, we observe two different karst types, according to drilling results. In the western part of the basin, where the limestones appear on the surface, the merokarst type is observed and water flow is limited in separated karstic conduits. On the contrary, in the central part of the basin, where the limestones underlie the clastic post-alpidic formations, the holokarst type is observed and a rich karstic aquifer is developed. This is explained by the closed hydraulic conditions. In the western part of the basin the karstic aquifer is unconfined, while in the central part it is confined, due to the overlying impermeable post-alpidic sediments and the overall closure of underground flow to the south. It appears that the confined conditions led to the development from merokarst to holokarst in this region.
Λεπτομέρειες άρθρου
- Πώς να δημιουργήσετε Αναφορές
-
Mariolakos, I., & Spyridonos, E. (2010). REMARKS ON THE KARSTIFICATION IN THE WIDER AREA OF THE UPPER MESSINIA CLOSED HYDROGEOLOGICAL BASIN (SW PELOPONNESUS, GREECE). Δελτίο της Ελληνικής Γεωλογικής Εταιρείας, 43(4), 1785–1791. https://doi.org/10.12681/bgsg.11364
- Ενότητα
- Υδρολογία και Υδρογεωλογία
Αυτή η εργασία είναι αδειοδοτημένη υπό το CC Αναφορά Δημιουργού – Μη Εμπορική Χρήση 4.0.
Οι συγγραφείς θα πρέπει να είναι σύμφωνοι με τα παρακάτω: Οι συγγραφείς των άρθρων που δημοσιεύονται στο περιοδικό διατηρούν τα δικαιώματα πνευματικής ιδιοκτησίας επί των άρθρων τους, δίνοντας στο περιοδικό το δικαίωμα της πρώτης δημοσίευσης. Άρθρα που δημοσιεύονται στο περιοδικό διατίθενται με άδεια Creative Commons 4.0 Non Commercial και σύμφωνα με την οποία μπορούν να χρησιμοποιούνται ελεύθερα, με αναφορά στο/στη συγγραφέα και στην πρώτη δημοσίευση για μη κερδοσκοπικούς σκοπούς. Οι συγγραφείς μπορούν να: Μοιραστούν — αντιγράψουν και αναδιανέμουν το υλικό με κάθε μέσο και τρόπο, Προσαρμόσουν — αναμείξουν, τροποποιήσουν και δημιουργήσουν πάνω στο υλικό.
Λήψεις
Τα δεδομένα λήψης δεν είναι ακόμη διαθέσιμα.
Αναφορές
Cvijič J. (1926). Das Karstphänomen, Pencks geograph., Wien, Abh. 5,3, 279p.
Fountoulis, Ι., (1994). Neotectonic evolution of Central-West Peloponnesus. Phd Theses, National and
Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, GΑΙΑ 7, 386 p.p. (in
Greek with English abstract).
Katsikatsos, G. (1980). Geological Study of the Vasiliko – Ithomi region, Messinia. I.G.M.E., GeologiXLIII,
No 4 – 1790
cal and Geophysical Studies, v. XXI, Nr. 1, 176 p, 12 plates, Athens (in Greek).
Lalechos, N. (1974). Geological Structure of Central-Western Peloponnesus. I.G.M.E., Geological recognisions,
Nr. 53, 94 p., 17 plates, Athens (in Greek).
Marcopoulou-Diacantoni, Α., Mirkou, Μ.-Α., Mariolakos, Ι., Fountoulis, Ι. (1991). Stratigraphic and
paleogeograph.ic observations at the post-alpine sediments of the Filiatra area (SW Peloponnesus,
Greece), and their neotectonic interpretation. - Βull. Gr. Geol. Soc., v. XXV/2, p. 593-608, Thessaloniki,
(in Greek).
Marcopoulou-Diacantoni, Α., Mirkou, Μ-R., Mariolakos, Ι., Logos, Ε., Lozios, S., Fountoulis, Ι. (1989).
Stratigraphic observations at the post-alpine of the Thouria-Ano Amphia (SW Peloponnesus, Greece),
and their neotectonic interpretation. - Βυll. Geol. Soc. Greece, ν. ΧΧΙΙΙ/3, ρ. 275-295, Athens, (in
Greek).
Mariolakos, I. (1988). The application of the Darcy’s Law in closed geomorphological and hydrogeological
systems, Example: the basin of Ano Messinia (SW Peloponnisos). In: Proceedings of the 3rd
Congress of the Geol. Soc. of Greece, Bull. Gr. Geol. Soc.,v. ΧΧ/3, 77-96, Athens (in Greek).
Mariolakos, Ι., Sabot, V., Alexopoulos, Α., Danamos, G., Lekkas, Ε., Logos, Ε., Lozios, S., Mertzanis,
Α., Fountoulis, Ι. (1987). Microzonic study of Kalamata (SW Peloponnesus, Greece), (Geomorphology,
Geology, Neotectonics). - Earth Planning Protection Organization, Report, 110ρ., Athens,
(in Greek).
Mariolakos, Ι., Fountoulis, Ι., Logos, Ε., Lozios, S. (1989). Surface faulting caused by the Kalamata
(Greece) earthquakes (13-9-1986). - Tectonophysics, 163, p. 197-203.
Mariolakos, Ι., Fountoulis, Ι., Marcopoulou-Diacantoni, Α., Mirkou, Μ.-R. (1994). Some remarks οη the
cinematic evolution of Messinia province (SW Peloponnesus, Greece) during the Pleistocene, based
οη neotectonic, stratigraphic and paleoecological observations. Munster. Forsch. Geol. Palaont. 76,
ρ. 371-380, Münster.
Mariolakos I., Lozios S. And Logos E. (1995). The neotectonic macrostructure of southern Peloponnesus.
The earthquakes of September 13, 1986. Seminar on active faults, XV Congress of the Carpatho-Balcan
Geological Association, 51-60, Athens.
Mariolakos, I., Fountoulis, I. & Ladas, I. (2001). The paleogeographic evolution of SW Peloponnese during
Quaternary period. In: Proceedings of the 9th Congress Geol. Soc. Greece, Bull. Geol. Soc.
Greece, v. XXXIV/1 pp. 37-45, (In Greek with English abstract).
Spyridonos, E., (1994). Simulation of the phreatic aquifer of the Ano Messini basin (SW Peloponnesus)
using mathematical modeling. In: Proceedings of the 7th Congress of the Geol. Soc. of Greece, Bull.
Gr. Geol. Soc., XXX/4, pp. 275-283, Thessaloniki (in Greek).
