{"id":{"repo_id":"greece","oai_identifier":"oai:10442/0223"},"canonical_url":"https://search.dev.ndltd.org/etd/greece/oai:10442/0223","repository":{"repo_id":"greece","name":"Greek National Archive of PhD Theses","base_url":"https://phdtheses.ekt.gr/eadd_oai/request"},"display":{"title":"ΝΕΟΤΕΚΤΟΝΙΚΗ ΕΞΕΛΙΞΗ ΤΗΣ ΛΕΚΑΝΗΣ ΦΛΩΡΙΝΑΣ-ΒΕΓΟΡΙΤΙΔΑΣ-ΠΤΟΛΕΜΑΙΔΑΣ (Δ. ΜΑΚΕΔΟΝΙΑ)","abstract":"NEOTECTONIC ANALYSIS OF NEOGENE AND QUATERNARY FAULTS IN THE FLORINA- VEGORITIS-PTOLEMAIS BASIN OF NW MACEDONIA (GREECE) LEADS TO THE CONCLUSION THAT TWO EXTENSIONAL PHASES CAN BE DISTINGUISHED. THE FIRST ONE, WITH A NNE-SSW STRESS DIRECTION, TOOK PLACE DURING LATE MIOCENE- PLIOCENE TIMES AND WAS RESPONSIBLE FOR THE INITIAL CREATION OF THE MAIN GRABEN SYSTEM OF THE FLORINA-VEGORITIS-PTOLEMAIS-KOZANI BASIN WHICH DEVELOPED WITH NORMAL FAULTS STRIKING NW-SE. THE SECONDPHASE, WITH A NW-SE DIRECTION, TOOK PLACE IN THE QUATERNARY AND WAS RESPONSIBLE FOR THE RECENT SUBBASINS AND RIDGES WHICH DEVELOPED ALONG NORMAL FAULTS STRIKING NE-SW. THE PLIO-QUATERNARY TENSIONAL STRESS-PATTERN OBTAINED FROM THE QUANTITATIVE ANALYSIS OF THE FAULTS IS CORRELATED WITH THE RESULTS OF PREVIOUS NEOTECTONIC STUDIES IN THE GREATER AEGEAN AREA.","abstract_html":"NEOTECTONIC ANALYSIS OF NEOGENE AND QUATERNARY FAULTS IN THE FLORINA- VEGORITIS-PTOLEMAIS BASIN OF NW MACEDONIA (GREECE) LEADS TO THE CONCLUSION THAT TWO EXTENSIONAL PHASES CAN BE DISTINGUISHED. THE FIRST ONE, WITH A NNE-SSW STRESS DIRECTION, TOOK PLACE DURING LATE MIOCENE- PLIOCENE TIMES AND WAS RESPONSIBLE FOR THE INITIAL CREATION OF THE MAIN GRABEN SYSTEM OF THE FLORINA-VEGORITIS-PTOLEMAIS-KOZANI BASIN WHICH DEVELOPED WITH NORMAL FAULTS STRIKING NW-SE. THE SECONDPHASE, WITH A NW-SE DIRECTION, TOOK PLACE IN THE QUATERNARY AND WAS RESPONSIBLE FOR THE RECENT SUBBASINS AND RIDGES WHICH DEVELOPED ALONG NORMAL FAULTS STRIKING NE-SW. THE PLIO-QUATERNARY TENSIONAL STRESS-PATTERN OBTAINED FROM THE QUANTITATIVE ANALYSIS OF THE FAULTS IS CORRELATED WITH THE RESULTS OF PREVIOUS NEOTECTONIC STUDIES IN THE GREATER AEGEAN AREA.","abstract_has_math":false,"creators":["Παυλίδης, Σπύρος","Pavlides, Spyros"],"institution":"Aristotle University Of Thessaloniki (AUTH)","degree_name":null,"degree_level":null,"degree_discipline":null,"degree_department":null,"school":null,"contributors":[],"advisors":[],"committee_chairs":[],"committee_members":[],"year":1985,"date_issued":"1985","date_published":"1985","updated_at":"2026-07-24T02:25:08Z","subjects":["Γεωλογία","ΓΕΩΤΕΚΤΟΝΙΚΗ","ΕΝΕΡΓΟΣ ΤΕΚΤΟΝΙΚΗ","ΕΦΕΛΚΥΣΤΙΚΗ ΤΕΚΤΟΝΙΚΗ","Μορφοτεκτονική","ΝΕΟΓΕΝΕΣ-ΤΕΤΑΡΤΟΓΕΝΕΣ","Νεοτεκτονική","ΠΕΛΑΓΩΝΙΚΗ","ΤΑΣΕΙΣ ΤΕΚΤΟΝΙΚΕΣ","ΤΕΚΤΟΝΙΚΗ ΓΕΩΛΟΓΙΑ","Tectonics, Active","EXTENSIONAL TECTONICS","Morphotectonics","NEOGENE BASIN OF PTOLEMAIS","Neotectonics","NEOTECTONICS OF AEGEAN AREA","NW NACEDONIA GREECE","STRESS PATTERN","Structural analysis","STRUCTURAL GEOLOGY"],"languages":["gre"],"rights":[],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier","label":"Identifier","values":["10.12681/eadd/0223"],"render_values":[{"text":"10.12681/eadd/0223","href":"https://doi.org/10.12681/eadd/0223","code":true}]}]},"links":{"outbound_url":"http://hdl.handle.net/10442/hedi/0223","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:creator","label":"Author","values":["Παυλίδης, Σπύρος","Pavlides, Spyros"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["1985"]},{"key":"dc:publisher","label":"Institution","values":["Aristotle University Of Thessaloniki (AUTH)","Αριστοτέλειο Πανεπιστήμιο Θεσσαλονίκης (ΑΠΘ)"]},{"key":"dc:type","label":"Dc Type","values":["PhD Thesis"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["Γεωλογία","ΓΕΩΤΕΚΤΟΝΙΚΗ","ΕΝΕΡΓΟΣ ΤΕΚΤΟΝΙΚΗ","ΕΦΕΛΚΥΣΤΙΚΗ ΤΕΚΤΟΝΙΚΗ","Μορφοτεκτονική","ΝΕΟΓΕΝΕΣ-ΤΕΤΑΡΤΟΓΕΝΕΣ","Νεοτεκτονική","ΠΕΛΑΓΩΝΙΚΗ","ΤΑΣΕΙΣ ΤΕΚΤΟΝΙΚΕΣ","ΤΕΚΤΟΝΙΚΗ ΓΕΩΛΟΓΙΑ","Tectonics, Active","EXTENSIONAL TECTONICS","Morphotectonics","NEOGENE BASIN OF PTOLEMAIS","Neotectonics","NEOTECTONICS OF AEGEAN AREA","NW NACEDONIA GREECE","STRESS PATTERN","Structural analysis","STRUCTURAL GEOLOGY"]}]},{"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/0223","http://hdl.handle.net/10442/hedi/0223"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["NEOTECTONIC ANALYSIS OF NEOGENE AND QUATERNARY FAULTS IN THE FLORINA- VEGORITIS-PTOLEMAIS BASIN OF NW MACEDONIA (GREECE) LEADS TO THE CONCLUSION THAT TWO EXTENSIONAL PHASES CAN BE DISTINGUISHED. THE FIRST ONE, WITH A NNE-SSW STRESS DIRECTION, TOOK PLACE DURING LATE MIOCENE- PLIOCENE TIMES AND WAS RESPONSIBLE FOR THE INITIAL CREATION OF THE MAIN GRABEN SYSTEM OF THE FLORINA-VEGORITIS-PTOLEMAIS-KOZANI BASIN WHICH DEVELOPED WITH NORMAL FAULTS STRIKING NW-SE. THE SECONDPHASE, WITH A NW-SE DIRECTION, TOOK PLACE IN THE QUATERNARY AND WAS RESPONSIBLE FOR THE RECENT SUBBASINS AND RIDGES WHICH DEVELOPED ALONG NORMAL FAULTS STRIKING NE-SW. THE PLIO-QUATERNARY TENSIONAL STRESS-PATTERN OBTAINED FROM THE QUANTITATIVE ANALYSIS OF THE FAULTS IS CORRELATED WITH THE RESULTS OF PREVIOUS NEOTECTONIC STUDIES IN THE GREATER AEGEAN AREA.","Η ΝΕΟΤΕΚΤΟΝΙΚΗ ΑΝΑΛΥΣΗ ΤΩΝ ΝΕΟΓΕΝΩΝ ΚΑΙ ΤΕΤΑΡΤΟΓΕΝΩΝ ΡΗΓΜΑΤΩΝ ΣΤΗΝ ΛΕΚΑΝΗ ΦΛΩΡΙΝΑΣ-ΒΕΓΟΡΙΤΙΔΑΣ-ΠΤΟΛΕΜΑΙΔΑΣ (ΒΔ ΜΑΚΕΔΟΝΙΑ) ΟΔΗΓΕΙ ΣΤΟ ΣΥΜΠΕΡΑΣΜΑ ΟΤΙ ΜΠΟΡΟΥΝ ΝΑ ΔΙΑΚΡΙΘΟΥΝ ΔΥΟ ΕΦΕΛΚΥΣΤΙΚΕΣ ΤΕΚΤΟΦΑΣΕΙΣ ΣΤΗΝ ΠΕΡΙΟΧΗ. Η ΠΡΩΤΗ, ΜΕ ΜΙΑ ΓΕΝΙΚΗ ΒΒΑ-ΝΝΔ ΔΙΕΥΘΥΝΣΗ ΤΩΝ ΤΑΣΕΩΝ, ΣΥΝΕΒΗ ΚΑΤΑ ΤΗ ΔΙΑΡΚΕΙΑ ΤΟΥ ΑΝΩΤΕΡΟΥ ΜΕΙΟΚΑΙΝΟΥ-ΠΛΕΙΟΚΑΙΝΟΥ ΚΑΙ ΗΤΑΝ ΥΠΕΥΘΥΝΗ ΓΙΑ ΤΗΝ ΑΡΧΙΚΗ ΔΗΜΙΟΥΡΓΙΑ ΤΟΥ ΚΥΡΙΟΥ ΒΥΘΙΣΜΑΤΟΣ ΤΗΣ ΦΛΩΡΙΝΑΣ- ΠΤΟΛΕΜΑΙΔΑΣ-ΚΟΖΑΝΗΣ, ΤΟ ΟΠΟΙΟ ΑΝΑΠΤΥΧΘΗΚΕ ΜΕ ΚΑΝΟΝΙΚΑ ΡΗΓΜΑΤΑ ΒΔ-ΝΑ ΔΙΕΥΘΥΝΣΗΣ. Η ΔΕΥΤΕΡΗ ΦΑΣΗ, ΜΕ ΜΙΑ ΒΔ-ΝΑ ΔΙΕΥΘΥΝΣΗ ΤΩΝ ΚΥΡΙΩΝ ΕΦΕΛΚΥΣΤΙΚΩΝ ΑΞΟΝΩΝ ΤΑΣΗΣ, ΣΥΝΕΒΗ ΚΑΤΑ ΤΟ ΤΕΤΑΡΤΟΓΕΝΕΣ ΚΑΙ ΗΤΑΝ ΥΠΕΥΘΥΝΗ ΓΙΑ ΤΗ ΔΗΜΙΟΥΡΓΙΑ ΤΩΝ ΠΡΟΣΦΑΤΩΝ ΜΙΚΡΟΤΕΡΩΝ ΥΠΟΛΕΚΑΝΩΝ ΚΑΙ ΕΦΑΡΜΑΤΩΝ, ΤΑ ΟΠΟΙΑ ΔΙΑΣΧΙΖΟΥΝ ΣΧΕΔΟΝ ΚΑΘΕΤΑ ΤΟ ΑΡΧΙΚΟ ΒΥΘΙΣΜΑ ΚΑΙ ΟΡΙΟΘΕΤΟΥΝΤΑΙ ΑΠΟ ΒΑ-ΝΔ ΚΑΝΟΝΙΚΑ ΡΗΓΜΑΤΑ. ΤΕΛΟΣ, ΣΤΗΝ ΕΡΓΑΣΙΑ ΑΥΤΗ ΓΙΝΕΤΑΙ ΜΙΑ ΠΡΟΣΠΑΘΕΙΑ ΩΣΤΕ ΤΟ ΕΦΕΛΚΥΣΤΙΚΟ ΠΕΔΙΟ ΤΩΝ ΤΑΣΕΩΝ ΤΟΥ ΠΛΕΙΟΤΕΤΑΡΤΟΓΕΝΟΥΣ, ΟΠΩΣ ΠΡΟΣΔΙΟΡΙΣΤΗΚΕ ΑΠΟ ΤΗΝ ΠΟΣΟΤΙΚΗ ΤΕΚΤΟΝΙΚΗ ΑΝΑΛΥΣΗ, ΝΑ ΣΥΓΚΡΙΘΕΙ ΚΑΙ ΝΑ ΣΥΣΧΕΤΙΣΘΕΙ ΜΕ ΤΑ ΑΠΟΤΕΛΕΣΜΑΤΑ ΠΡΟΗΓΟΥΜΕΝΩΝ ΑΝΑΛΟΓΩΝΝΕΟΤΕΚΤΟΝΙΚΩΝ ΕΡΓΑΣΙΩΝ ΤΗΣ ΕΥΡΥΤΕΡΗΣ ΠΕΡΙΟΧΗΣ ΤΟΥ ΑΙΓΑΙΟΥ."]},{"key":"dc:title","label":"Title","values":["ΝΕΟΤΕΚΤΟΝΙΚΗ ΕΞΕΛΙΞΗ ΤΗΣ ΛΕΚΑΝΗΣ ΦΛΩΡΙΝΑΣ-ΒΕΓΟΡΙΤΙΔΑΣ-ΠΤΟΛΕΜΑΙΔΑΣ (Δ. ΜΑΚΕΔΟΝΙΑ)","NEOTECTONIC EVOLUTION OF THE FLORINA-VEGORITIS-PTOLEMAIS BASIN (W. MACEDONIA, GREECE)"]}]}],"canonical_facts":{"dc:creator":["Παυλίδης, Σπύρος","Pavlides, Spyros"],"dc:date":["1985"],"dc:description":["NEOTECTONIC ANALYSIS OF NEOGENE AND QUATERNARY FAULTS IN THE FLORINA- VEGORITIS-PTOLEMAIS BASIN OF NW MACEDONIA (GREECE) LEADS TO THE CONCLUSION THAT TWO EXTENSIONAL PHASES CAN BE DISTINGUISHED. THE FIRST ONE, WITH A NNE-SSW STRESS DIRECTION, TOOK PLACE DURING LATE MIOCENE- PLIOCENE TIMES AND WAS RESPONSIBLE FOR THE INITIAL CREATION OF THE MAIN GRABEN SYSTEM OF THE FLORINA-VEGORITIS-PTOLEMAIS-KOZANI BASIN WHICH DEVELOPED WITH NORMAL FAULTS STRIKING NW-SE. THE SECONDPHASE, WITH A NW-SE DIRECTION, TOOK PLACE IN THE QUATERNARY AND WAS RESPONSIBLE FOR THE RECENT SUBBASINS AND RIDGES WHICH DEVELOPED ALONG NORMAL FAULTS STRIKING NE-SW. THE PLIO-QUATERNARY TENSIONAL STRESS-PATTERN OBTAINED FROM THE QUANTITATIVE ANALYSIS OF THE FAULTS IS CORRELATED WITH THE RESULTS OF PREVIOUS NEOTECTONIC STUDIES IN THE GREATER AEGEAN AREA.","Η ΝΕΟΤΕΚΤΟΝΙΚΗ ΑΝΑΛΥΣΗ ΤΩΝ ΝΕΟΓΕΝΩΝ ΚΑΙ ΤΕΤΑΡΤΟΓΕΝΩΝ ΡΗΓΜΑΤΩΝ ΣΤΗΝ ΛΕΚΑΝΗ ΦΛΩΡΙΝΑΣ-ΒΕΓΟΡΙΤΙΔΑΣ-ΠΤΟΛΕΜΑΙΔΑΣ (ΒΔ ΜΑΚΕΔΟΝΙΑ) ΟΔΗΓΕΙ ΣΤΟ ΣΥΜΠΕΡΑΣΜΑ ΟΤΙ ΜΠΟΡΟΥΝ ΝΑ ΔΙΑΚΡΙΘΟΥΝ ΔΥΟ ΕΦΕΛΚΥΣΤΙΚΕΣ ΤΕΚΤΟΦΑΣΕΙΣ ΣΤΗΝ ΠΕΡΙΟΧΗ. Η ΠΡΩΤΗ, ΜΕ ΜΙΑ ΓΕΝΙΚΗ ΒΒΑ-ΝΝΔ ΔΙΕΥΘΥΝΣΗ ΤΩΝ ΤΑΣΕΩΝ, ΣΥΝΕΒΗ ΚΑΤΑ ΤΗ ΔΙΑΡΚΕΙΑ ΤΟΥ ΑΝΩΤΕΡΟΥ ΜΕΙΟΚΑΙΝΟΥ-ΠΛΕΙΟΚΑΙΝΟΥ ΚΑΙ ΗΤΑΝ ΥΠΕΥΘΥΝΗ ΓΙΑ ΤΗΝ ΑΡΧΙΚΗ ΔΗΜΙΟΥΡΓΙΑ ΤΟΥ ΚΥΡΙΟΥ ΒΥΘΙΣΜΑΤΟΣ ΤΗΣ ΦΛΩΡΙΝΑΣ- ΠΤΟΛΕΜΑΙΔΑΣ-ΚΟΖΑΝΗΣ, ΤΟ ΟΠΟΙΟ ΑΝΑΠΤΥΧΘΗΚΕ ΜΕ ΚΑΝΟΝΙΚΑ ΡΗΓΜΑΤΑ ΒΔ-ΝΑ ΔΙΕΥΘΥΝΣΗΣ. Η ΔΕΥΤΕΡΗ ΦΑΣΗ, ΜΕ ΜΙΑ ΒΔ-ΝΑ ΔΙΕΥΘΥΝΣΗ ΤΩΝ ΚΥΡΙΩΝ ΕΦΕΛΚΥΣΤΙΚΩΝ ΑΞΟΝΩΝ ΤΑΣΗΣ, ΣΥΝΕΒΗ ΚΑΤΑ ΤΟ ΤΕΤΑΡΤΟΓΕΝΕΣ ΚΑΙ ΗΤΑΝ ΥΠΕΥΘΥΝΗ ΓΙΑ ΤΗ ΔΗΜΙΟΥΡΓΙΑ ΤΩΝ ΠΡΟΣΦΑΤΩΝ ΜΙΚΡΟΤΕΡΩΝ ΥΠΟΛΕΚΑΝΩΝ ΚΑΙ ΕΦΑΡΜΑΤΩΝ, ΤΑ ΟΠΟΙΑ ΔΙΑΣΧΙΖΟΥΝ ΣΧΕΔΟΝ ΚΑΘΕΤΑ ΤΟ ΑΡΧΙΚΟ ΒΥΘΙΣΜΑ ΚΑΙ ΟΡΙΟΘΕΤΟΥΝΤΑΙ ΑΠΟ ΒΑ-ΝΔ ΚΑΝΟΝΙΚΑ ΡΗΓΜΑΤΑ. ΤΕΛΟΣ, ΣΤΗΝ ΕΡΓΑΣΙΑ ΑΥΤΗ ΓΙΝΕΤΑΙ ΜΙΑ ΠΡΟΣΠΑΘΕΙΑ ΩΣΤΕ ΤΟ ΕΦΕΛΚΥΣΤΙΚΟ ΠΕΔΙΟ ΤΩΝ ΤΑΣΕΩΝ ΤΟΥ ΠΛΕΙΟΤΕΤΑΡΤΟΓΕΝΟΥΣ, ΟΠΩΣ ΠΡΟΣΔΙΟΡΙΣΤΗΚΕ ΑΠΟ ΤΗΝ ΠΟΣΟΤΙΚΗ ΤΕΚΤΟΝΙΚΗ ΑΝΑΛΥΣΗ, ΝΑ ΣΥΓΚΡΙΘΕΙ ΚΑΙ ΝΑ ΣΥΣΧΕΤΙΣΘΕΙ ΜΕ ΤΑ ΑΠΟΤΕΛΕΣΜΑΤΑ ΠΡΟΗΓΟΥΜΕΝΩΝ ΑΝΑΛΟΓΩΝΝΕΟΤΕΚΤΟΝΙΚΩΝ ΕΡΓΑΣΙΩΝ ΤΗΣ ΕΥΡΥΤΕΡΗΣ ΠΕΡΙΟΧΗΣ ΤΟΥ ΑΙΓΑΙΟΥ."],"dc:identifier":["10.12681/eadd/0223","http://hdl.handle.net/10442/hedi/0223"],"dc:language":["gre"],"dc:publisher":["Aristotle University Of Thessaloniki (AUTH)","Αριστοτέλειο Πανεπιστήμιο Θεσσαλονίκης (ΑΠΘ)"],"dc:subject":["Γεωλογία","ΓΕΩΤΕΚΤΟΝΙΚΗ","ΕΝΕΡΓΟΣ ΤΕΚΤΟΝΙΚΗ","ΕΦΕΛΚΥΣΤΙΚΗ ΤΕΚΤΟΝΙΚΗ","Μορφοτεκτονική","ΝΕΟΓΕΝΕΣ-ΤΕΤΑΡΤΟΓΕΝΕΣ","Νεοτεκτονική","ΠΕΛΑΓΩΝΙΚΗ","ΤΑΣΕΙΣ ΤΕΚΤΟΝΙΚΕΣ","ΤΕΚΤΟΝΙΚΗ ΓΕΩΛΟΓΙΑ","Tectonics, Active","EXTENSIONAL TECTONICS","Morphotectonics","NEOGENE BASIN OF PTOLEMAIS","Neotectonics","NEOTECTONICS OF AEGEAN AREA","NW NACEDONIA GREECE","STRESS PATTERN","Structural analysis","STRUCTURAL GEOLOGY"],"dc:title":["ΝΕΟΤΕΚΤΟΝΙΚΗ ΕΞΕΛΙΞΗ ΤΗΣ ΛΕΚΑΝΗΣ ΦΛΩΡΙΝΑΣ-ΒΕΓΟΡΙΤΙΔΑΣ-ΠΤΟΛΕΜΑΙΔΑΣ (Δ. ΜΑΚΕΔΟΝΙΑ)","NEOTECTONIC EVOLUTION OF THE FLORINA-VEGORITIS-PTOLEMAIS BASIN (W. MACEDONIA, GREECE)"],"dc:type":["PhD Thesis"]},"updated_at":"2026-07-24T02:25:08Z"}