{"id":{"repo_id":"greece","oai_identifier":"oai:10442/1738"},"canonical_url":"https://search.dev.ndltd.org/etd/greece/oai:10442/1738","repository":{"repo_id":"greece","name":"Greek National Archive of PhD Theses","base_url":"https://phdtheses.ekt.gr/eadd_oai/request"},"display":{"title":"ΟΙ ΥΔΡΟΓΕΩΛΟΓΙΚΕΣ ΣΥΝΘΗΚΕΣ ΤΩΝ ΚΑΡΣΤΙΚΩΝ ΚΑΙ ΝΕΟΓΕΝΩΝ ΣΥΣΤΗΜΑΤΩΝ ΤΗΣ ΛΕΚΑΝΗΣ ΜΟΛΑΩΝ (ΛΑΚΩΝΙΑ)","abstract":"VERTICAL MOVEMENTS OCCURED DURING THE NEOGENE IN THE AREA OF STUDY FOLLOWING THE DIRECTION OF OLDER FAULTS (VIZ. NNW TO NW AND NNE TO NE). THUS GRABENS AND HORSTS WERE CREATED (E.G. MOLAI GRABEN, ASOPOS HORST, PLYTRA GRABEN. THERE WERE RECOGNISED FOUR KARSTIC EROSIONAL SURFACES. THE GEOLOGIC FORMATIONS OUTCROPPING IN THE MOLAI AREA ARE THE FOLLOWING: A) PHYLLITE-QUARTZITE SERIES, B) TYROS BEDS, C) TRIPOLITSA LIMESTONES, D) OLONOS ZONE, E) PELAGONIAN ZONE, F) THIC NEOGENE SEDIMENTS, THE EQUATION EXPRESSING THE RELATION BETWEEN ALTITUDE (X) AND PRECIPITATION (Y) WAS Y=0.573X + 588,5. THE WATERS OF THE KARST AQUIFER DISCHARGE THROUGH THE COASTAL SUBMARINE SPRINGS OF GLYFADA WITH A RATE OF 1.3 L/S. SEA WATER INTRUSION IN THE KARST AQUIFER OCCURS VIA NNW AND NW STRIKING FAULTS, WHILE IN THE NEOGENE AQUIFER DUE TO OVERPUMPING OF THE DRILLED BOREHOLES SOUTH OF ASOPOS.","abstract_html":"VERTICAL MOVEMENTS OCCURED DURING THE NEOGENE IN THE AREA OF STUDY FOLLOWING THE DIRECTION OF OLDER FAULTS (VIZ. NNW TO NW AND NNE TO NE). THUS GRABENS AND HORSTS WERE CREATED (E.G. MOLAI GRABEN, ASOPOS HORST, PLYTRA GRABEN. THERE WERE RECOGNISED FOUR KARSTIC EROSIONAL SURFACES. THE GEOLOGIC FORMATIONS OUTCROPPING IN THE MOLAI AREA ARE THE FOLLOWING: A) PHYLLITE-QUARTZITE SERIES, B) TYROS BEDS, C) TRIPOLITSA LIMESTONES, D) OLONOS ZONE, E) PELAGONIAN ZONE, F) THIC NEOGENE SEDIMENTS, THE EQUATION EXPRESSING THE RELATION BETWEEN ALTITUDE (X) AND PRECIPITATION (Y) WAS Y=0.573X + 588,5. THE WATERS OF THE KARST AQUIFER DISCHARGE THROUGH THE COASTAL SUBMARINE SPRINGS OF GLYFADA WITH A RATE OF 1.3 L/S. SEA WATER INTRUSION IN THE KARST AQUIFER OCCURS VIA NNW AND NW STRIKING FAULTS, WHILE IN THE NEOGENE AQUIFER DUE TO OVERPUMPING OF THE DRILLED BOREHOLES SOUTH OF ASOPOS.","abstract_has_math":false,"creators":["Ταβιτιάν, Καραμπέτ"],"institution":"Πανεπιστήμιο Πατρών","degree_name":null,"degree_level":null,"degree_discipline":null,"degree_department":null,"school":null,"contributors":[],"advisors":[],"committee_chairs":[],"committee_members":[],"year":1991,"date_issued":"1991","date_published":"1991","updated_at":"2026-07-24T02:25:05Z","subjects":["Aquifers","Hydrogeology","Hydrology","Karst","Neogene","Water chemistry","Καρστ","ΝΕΟΓΕΝΗ","Υδρογεωλογία","ΥΔΡΟΛΙΘΟΛΟΓΙΑ-ΥΔΡΟΦΟΡΑ","Υδρολογία","Υδροχημεία","Φυσικές Επιστήμες","Natural Sciences","Γεωεπιστήμες και Επιστήμες Περιβάλλοντος","Earth and Related Environmental Sciences"],"languages":["gre"],"rights":[],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier","label":"Identifier","values":["10.12681/eadd/1738"],"render_values":[{"text":"10.12681/eadd/1738","href":"https://doi.org/10.12681/eadd/1738","code":true}]}]},"links":{"outbound_url":"http://hdl.handle.net/10442/hedi/1738","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:creator","label":"Author","values":["Ταβιτιάν, Καραμπέτ"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["1991"]},{"key":"dc:publisher","label":"Institution","values":["Πανεπιστήμιο Πατρών","University of Patras"]},{"key":"dc:type","label":"Dc Type","values":["PhD Thesis"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["Aquifers","Hydrogeology","Hydrology","Karst","Neogene","Water chemistry","Καρστ","ΝΕΟΓΕΝΗ","Υδρογεωλογία","ΥΔΡΟΛΙΘΟΛΟΓΙΑ-ΥΔΡΟΦΟΡΑ","Υδρολογία","Υδροχημεία","Φυσικές Επιστήμες","Natural Sciences","Γεωεπιστήμες και Επιστήμες Περιβάλλοντος","Earth and Related Environmental Sciences"]}]},{"id":"language_rights","label":"Language and Rights","entries":[{"key":"dc:language","label":"Dc Language","values":["gre"]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier","label":"Identifier","values":["10.12681/eadd/1738","http://hdl.handle.net/10442/hedi/1738"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["VERTICAL MOVEMENTS OCCURED DURING THE NEOGENE IN THE AREA OF STUDY FOLLOWING THE DIRECTION OF OLDER FAULTS (VIZ. NNW TO NW AND NNE TO NE). THUS GRABENS AND HORSTS WERE CREATED (E.G. MOLAI GRABEN, ASOPOS HORST, PLYTRA GRABEN. THERE WERE RECOGNISED FOUR KARSTIC EROSIONAL SURFACES. THE GEOLOGIC FORMATIONS OUTCROPPING IN THE MOLAI AREA ARE THE FOLLOWING: A) PHYLLITE-QUARTZITE SERIES, B) TYROS BEDS, C) TRIPOLITSA LIMESTONES, D) OLONOS ZONE, E) PELAGONIAN ZONE, F) THIC NEOGENE SEDIMENTS, THE EQUATION EXPRESSING THE RELATION BETWEEN ALTITUDE (X) AND PRECIPITATION (Y) WAS Y=0.573X + 588,5. THE WATERS OF THE KARST AQUIFER DISCHARGE THROUGH THE COASTAL SUBMARINE SPRINGS OF GLYFADA WITH A RATE OF 1.3 L/S. SEA WATER INTRUSION IN THE KARST AQUIFER OCCURS VIA NNW AND NW STRIKING FAULTS, WHILE IN THE NEOGENE AQUIFER DUE TO OVERPUMPING OF THE DRILLED BOREHOLES SOUTH OF ASOPOS.","ΚΑΤΑ ΤΗ ΔΙΑΡΚΕΙΑ ΤΟΥ ΝΕΟΓΕΝΟΥΣ ΕΓΙΝΑΝ ΣΤΗΝ ΠΕΡΙΟΧΗ ΜΟΛΑΩΝ ΣΧΕΔΟΝ ΚΑΤΑΚΟΡΥΦΕΣ ΜΕΤΑΚΙΝΗΣΕΙΣ ΑΚΟΛΟΥΘΩΝΤΑΣ ΤΗ ΔΙΕΥΘΥΝΣΗ ΤΩΝ ΠΑΛΑΙΟΤΕΡΩΝ ΡΗΓΜΑΤΩΝ (ΒΒΔ ΤΗΣ ΒΔ ΚΑΙ ΒΒΑ ΤΗΣ ΒΑ) ΚΑΙ ΕΙΧΑΝ ΩΣ ΑΠΟΤΕΛΕΣΜΑ ΤΗΝ ΔΗΜΙΟΥΡΓΙΑ ΤΕΚΤΟΝΙΚΩΝ ΤΑΦΡΩΝ ΚΑΙ ΚΕΡΑΤΩΝ(ΤΑΦΡΟΣ ΜΟΛΑΩΝ, ΚΕΡΑΣ ΑΣΩΠΟΥ ΚΑΙ ΤΑΦΡΟΣ ΠΛΥΤΡΑΣ). ΑΝΑΓΝΩΡΙΣΤΗΚΑΝ ΤΕΣΣΕΡΑ ΕΠΙΠΕΔΑ ΚΑΡΣΤΙΚΗΣ ΔΙΑΒΡΩΣΗΣ (ΧΙΟΝΟΒΟΥΝΙΟΥ, ΚΟΥΠΙΩΝ, ΝΙΑΤΩΝ ΚΑΙ ΠΑΛ. ΜΟΝΕΜΒΑΣΙΑΣ). ΣΤΗΝ ΠΕΡΙΟΧΗ ΜΕΛΕΤΗΣ ΑΠΑΝΤΩΝΤΑΙ ΟΙ ΕΞΗΣ ΓΕΩΛΟΓΙΚΟΙ ΣΧΗΜΑΤΙΣΜΟΙ: Α) ΣΕΙΡΑ ΦΥΛΛΙΤΩΝ-ΧΑΛΑΖΙΤΩΝ, Β) ΖΩΝΗ ΤΡΙΠΟΛΕΩΣ Γ) ΣΤΡΩΜΑΤΑ ΤΥΡΟΥ, Δ) ΖΩΝΗ ΟΛΟΝΟΥ, Ε) ΠΕΛΑΓΟΝΙΚΗ ΖΩΝΗ, ΣΤ) ΝΕΟΓΕΝΗ ΙΖΗΜΑΤΑ. ΤΟ ΥΨΟΣ ΥΕΤΟΥ (Ψ) ΕΠΗΡΕΑΖΕΤΑΙ ΚΥΡΙΩΣ ΑΠΟ ΤΟ ΥΨΟΜΕΤΡΟ(Χ) (Ψ=0.573Χ + 588.5). ΤΑ ΝΕΡΑ ΤΟΥ ΚΑΡΣΤΙΚΟΥ ΣΥΣΤΗΜΑΤΟΣ ΤΗΣ ΥΔΡΟΓΕΩΛΟΓΙΚΗΣ ΛΕΚΑΝΗΣ ΤΡΟΦΟΔΟΤΟΥΝ ΚΥΡΙΩΣ ΤΟ ΜΕΤΩΠΟ ΤΩΝ ΚΑΡΣΤΙΚΩΝ ΠΗΓΩΝ ΤΗΣ ΓΛΥΦΑΔΑΣ ΠΟΥ Η ΠΕΡΙΟΧΗ ΤΟΥΣ ΦΘΑΝΕΙ 41 Χ 106 Μ3/ΕΤΟΣ. Η ΥΦΑΛΜΥΡΩΣΗ ΤΟΥ ΚΑΡΣΤΙΚΟΥ ΥΔΡΟΦΟΡΟΥ ΓΙΝΕΤΑΙ ΜΕΣΩ ΤΩΝ ΒΒ4 ΤΗΣ Β4 ΡΗΓΜΑΤΩΝ, ΕΝΩ ΤΟΥ ΥΔΡΟΦΟΡΕΑ ΤΩΝ ΝΕΟΓΕΝΩΝ ΛΟΓΩ ΥΠΕΡΑΝΤΛΗΣΗΣ."]},{"key":"dc:title","label":"Title","values":["ΟΙ ΥΔΡΟΓΕΩΛΟΓΙΚΕΣ ΣΥΝΘΗΚΕΣ ΤΩΝ ΚΑΡΣΤΙΚΩΝ ΚΑΙ ΝΕΟΓΕΝΩΝ ΣΥΣΤΗΜΑΤΩΝ ΤΗΣ ΛΕΚΑΝΗΣ ΜΟΛΑΩΝ (ΛΑΚΩΝΙΑ)","HYDROGEOLOGICAL CONDITIONS OF THE KARSTIC AND NEOGENE SYSTEMS OF THE MOLAI BASIN-IN LACONIA-GREECE"]}]}],"canonical_facts":{"dc:creator":["Ταβιτιάν, Καραμπέτ"],"dc:date":["1991"],"dc:description":["VERTICAL MOVEMENTS OCCURED DURING THE NEOGENE IN THE AREA OF STUDY FOLLOWING THE DIRECTION OF OLDER FAULTS (VIZ. NNW TO NW AND NNE TO NE). THUS GRABENS AND HORSTS WERE CREATED (E.G. MOLAI GRABEN, ASOPOS HORST, PLYTRA GRABEN. THERE WERE RECOGNISED FOUR KARSTIC EROSIONAL SURFACES. THE GEOLOGIC FORMATIONS OUTCROPPING IN THE MOLAI AREA ARE THE FOLLOWING: A) PHYLLITE-QUARTZITE SERIES, B) TYROS BEDS, C) TRIPOLITSA LIMESTONES, D) OLONOS ZONE, E) PELAGONIAN ZONE, F) THIC NEOGENE SEDIMENTS, THE EQUATION EXPRESSING THE RELATION BETWEEN ALTITUDE (X) AND PRECIPITATION (Y) WAS Y=0.573X + 588,5. THE WATERS OF THE KARST AQUIFER DISCHARGE THROUGH THE COASTAL SUBMARINE SPRINGS OF GLYFADA WITH A RATE OF 1.3 L/S. SEA WATER INTRUSION IN THE KARST AQUIFER OCCURS VIA NNW AND NW STRIKING FAULTS, WHILE IN THE NEOGENE AQUIFER DUE TO OVERPUMPING OF THE DRILLED BOREHOLES SOUTH OF ASOPOS.","ΚΑΤΑ ΤΗ ΔΙΑΡΚΕΙΑ ΤΟΥ ΝΕΟΓΕΝΟΥΣ ΕΓΙΝΑΝ ΣΤΗΝ ΠΕΡΙΟΧΗ ΜΟΛΑΩΝ ΣΧΕΔΟΝ ΚΑΤΑΚΟΡΥΦΕΣ ΜΕΤΑΚΙΝΗΣΕΙΣ ΑΚΟΛΟΥΘΩΝΤΑΣ ΤΗ ΔΙΕΥΘΥΝΣΗ ΤΩΝ ΠΑΛΑΙΟΤΕΡΩΝ ΡΗΓΜΑΤΩΝ (ΒΒΔ ΤΗΣ ΒΔ ΚΑΙ ΒΒΑ ΤΗΣ ΒΑ) ΚΑΙ ΕΙΧΑΝ ΩΣ ΑΠΟΤΕΛΕΣΜΑ ΤΗΝ ΔΗΜΙΟΥΡΓΙΑ ΤΕΚΤΟΝΙΚΩΝ ΤΑΦΡΩΝ ΚΑΙ ΚΕΡΑΤΩΝ(ΤΑΦΡΟΣ ΜΟΛΑΩΝ, ΚΕΡΑΣ ΑΣΩΠΟΥ ΚΑΙ ΤΑΦΡΟΣ ΠΛΥΤΡΑΣ). ΑΝΑΓΝΩΡΙΣΤΗΚΑΝ ΤΕΣΣΕΡΑ ΕΠΙΠΕΔΑ ΚΑΡΣΤΙΚΗΣ ΔΙΑΒΡΩΣΗΣ (ΧΙΟΝΟΒΟΥΝΙΟΥ, ΚΟΥΠΙΩΝ, ΝΙΑΤΩΝ ΚΑΙ ΠΑΛ. ΜΟΝΕΜΒΑΣΙΑΣ). ΣΤΗΝ ΠΕΡΙΟΧΗ ΜΕΛΕΤΗΣ ΑΠΑΝΤΩΝΤΑΙ ΟΙ ΕΞΗΣ ΓΕΩΛΟΓΙΚΟΙ ΣΧΗΜΑΤΙΣΜΟΙ: Α) ΣΕΙΡΑ ΦΥΛΛΙΤΩΝ-ΧΑΛΑΖΙΤΩΝ, Β) ΖΩΝΗ ΤΡΙΠΟΛΕΩΣ Γ) ΣΤΡΩΜΑΤΑ ΤΥΡΟΥ, Δ) ΖΩΝΗ ΟΛΟΝΟΥ, Ε) ΠΕΛΑΓΟΝΙΚΗ ΖΩΝΗ, ΣΤ) ΝΕΟΓΕΝΗ ΙΖΗΜΑΤΑ. ΤΟ ΥΨΟΣ ΥΕΤΟΥ (Ψ) ΕΠΗΡΕΑΖΕΤΑΙ ΚΥΡΙΩΣ ΑΠΟ ΤΟ ΥΨΟΜΕΤΡΟ(Χ) (Ψ=0.573Χ + 588.5). ΤΑ ΝΕΡΑ ΤΟΥ ΚΑΡΣΤΙΚΟΥ ΣΥΣΤΗΜΑΤΟΣ ΤΗΣ ΥΔΡΟΓΕΩΛΟΓΙΚΗΣ ΛΕΚΑΝΗΣ ΤΡΟΦΟΔΟΤΟΥΝ ΚΥΡΙΩΣ ΤΟ ΜΕΤΩΠΟ ΤΩΝ ΚΑΡΣΤΙΚΩΝ ΠΗΓΩΝ ΤΗΣ ΓΛΥΦΑΔΑΣ ΠΟΥ Η ΠΕΡΙΟΧΗ ΤΟΥΣ ΦΘΑΝΕΙ 41 Χ 106 Μ3/ΕΤΟΣ. Η ΥΦΑΛΜΥΡΩΣΗ ΤΟΥ ΚΑΡΣΤΙΚΟΥ ΥΔΡΟΦΟΡΟΥ ΓΙΝΕΤΑΙ ΜΕΣΩ ΤΩΝ ΒΒ4 ΤΗΣ Β4 ΡΗΓΜΑΤΩΝ, ΕΝΩ ΤΟΥ ΥΔΡΟΦΟΡΕΑ ΤΩΝ ΝΕΟΓΕΝΩΝ ΛΟΓΩ ΥΠΕΡΑΝΤΛΗΣΗΣ."],"dc:identifier":["10.12681/eadd/1738","http://hdl.handle.net/10442/hedi/1738"],"dc:language":["gre"],"dc:publisher":["Πανεπιστήμιο Πατρών","University of Patras"],"dc:subject":["Aquifers","Hydrogeology","Hydrology","Karst","Neogene","Water chemistry","Καρστ","ΝΕΟΓΕΝΗ","Υδρογεωλογία","ΥΔΡΟΛΙΘΟΛΟΓΙΑ-ΥΔΡΟΦΟΡΑ","Υδρολογία","Υδροχημεία","Φυσικές Επιστήμες","Natural Sciences","Γεωεπιστήμες και Επιστήμες Περιβάλλοντος","Earth and Related Environmental Sciences"],"dc:title":["ΟΙ ΥΔΡΟΓΕΩΛΟΓΙΚΕΣ ΣΥΝΘΗΚΕΣ ΤΩΝ ΚΑΡΣΤΙΚΩΝ ΚΑΙ ΝΕΟΓΕΝΩΝ ΣΥΣΤΗΜΑΤΩΝ ΤΗΣ ΛΕΚΑΝΗΣ ΜΟΛΑΩΝ (ΛΑΚΩΝΙΑ)","HYDROGEOLOGICAL CONDITIONS OF THE KARSTIC AND NEOGENE SYSTEMS OF THE MOLAI BASIN-IN LACONIA-GREECE"],"dc:type":["PhD Thesis"]},"updated_at":"2026-07-24T02:25:05Z"}