{"id":{"repo_id":"greece","oai_identifier":"oai:10442/1531"},"canonical_url":"https://search.dev.ndltd.org/etd/greece/oai:10442/1531","repository":{"repo_id":"greece","name":"Greek National Archive of PhD Theses","base_url":"https://phdtheses.ekt.gr/eadd_oai/request"},"display":{"title":"ΣΥΜΒΟΛΗ ΤΗΣ ΠΟΣΟΤΙΚΗΣ ΜΕΛΕΤΗΣ ΤΩΝ ΥΔΡΟΓΡΑΦΙΚΩΝ ΣΥΣΤΗΜΑΤΩΝ ΣΤΗΝ ΠΑΛΑΙΟΓΕΩΓΡΑΦΙΚΗ ΕΞΕΛΙΞΗ ΤΩΝ ΟΡΕΩΝ ΤΗΣ ΒΟΛΒΗΣ","abstract":"THE AIM OF THE THESIS WAS THE DETECTION OF THE POSSIBLE STAGES OF THE DEVELOPMENT AND EVOLUTION OF THE DRAINAGE SYSTEMS ON VOLVI MOUNTAINS. THE DRAINAGE SYSTEMS WERE DRAWN FROM AIRPHOTOS AND WERE USED TO MEASURE AND CALCULATE PARAMETERS WHICH EXPRESS THE DIMENSION AND SHAPE OF THE BASINS, THE RELIEF, THE DEGREE OF DISSECTION AND THE AZIMUTHS OF THE STREAM SEGMENTS. THESE AZIMUTHS SHOWED HOW MUCH THE DRAINAGE NETWORK WAS INFLUENCED BY THE FAULT LINES. THE REST OF THE PARAMETERS STUDIED BY FACTOR ANALYSIS AND GAVE NEW EVIDENCES CONCERNING THE ROLE OF THE BASIN RELIEF ON THE FORMATION OF THE BASIN'S DIMENSIONS. ALSO, THREE ISOLINE MAPS WERE CONSTRUCTED PRESENTING THE EVOLUTION AND DEVELOPMENT OF THE DRAINAGE SYSTEMS AND PALAEORELIEF IN TWO SUCCESSIVELY STAGES.","abstract_html":"THE AIM OF THE THESIS WAS THE DETECTION OF THE POSSIBLE STAGES OF THE DEVELOPMENT AND EVOLUTION OF THE DRAINAGE SYSTEMS ON VOLVI MOUNTAINS. THE DRAINAGE SYSTEMS WERE DRAWN FROM AIRPHOTOS AND WERE USED TO MEASURE AND CALCULATE PARAMETERS WHICH EXPRESS THE DIMENSION AND SHAPE OF THE BASINS, THE RELIEF, THE DEGREE OF DISSECTION AND THE AZIMUTHS OF THE STREAM SEGMENTS. THESE AZIMUTHS SHOWED HOW MUCH THE DRAINAGE NETWORK WAS INFLUENCED BY THE FAULT LINES. THE REST OF THE PARAMETERS STUDIED BY FACTOR ANALYSIS AND GAVE NEW EVIDENCES CONCERNING THE ROLE OF THE BASIN RELIEF ON THE FORMATION OF THE BASIN&#x27;S DIMENSIONS. ALSO, THREE ISOLINE MAPS WERE CONSTRUCTED PRESENTING THE EVOLUTION AND DEVELOPMENT OF THE DRAINAGE SYSTEMS AND PALAEORELIEF IN TWO SUCCESSIVELY STAGES.","abstract_has_math":false,"creators":["Λαμπρινός, Νικόλαος","Lambrinos, Nikolaos"],"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":1989,"date_issued":"1989","date_published":"1989","updated_at":"2026-07-24T02:24:59Z","subjects":["ΜΗ ΠΑΡΑΜΕΤΡΙΚΗ ΣΤΑΤΙΣΤΙΚΗ","Παλαιογεωγραφική εξέλιξη","Παραγοντική ανάλυση","ΣΥΣΧΕΤΙΣΜΟΣ ΤΕΚΤΟΝΙΚΩΝ ΓΡΑΜΜΩΝ","ΣΥΣΧΕΤΙΣΜΟΣ ΥΔΡΟΓΡΑΦΙΚΩΝ ΣΥΣΤΗΜΑΤΩΝ","ΥΔΡΟΓΡΑΦΙΚΑ ΣΥΣΤΗΜΑΤΑ","AZIMUTHS OF STREAM SEGMENTS-FAULT LINEAMENTS","Drainage systems","Factor analysis","Palaeogeographical evolution","VOLVI MOUNTAINS-NORTH GREECE"],"languages":["gre"],"rights":[],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier","label":"Identifier","values":["10.12681/eadd/1531"],"render_values":[{"text":"10.12681/eadd/1531","href":"https://doi.org/10.12681/eadd/1531","code":true}]}]},"links":{"outbound_url":"http://hdl.handle.net/10442/hedi/1531","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:creator","label":"Author","values":["Λαμπρινός, Νικόλαος","Lambrinos, Nikolaos"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["1989"]},{"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":["ΜΗ ΠΑΡΑΜΕΤΡΙΚΗ ΣΤΑΤΙΣΤΙΚΗ","Παλαιογεωγραφική εξέλιξη","Παραγοντική ανάλυση","ΣΥΣΧΕΤΙΣΜΟΣ ΤΕΚΤΟΝΙΚΩΝ ΓΡΑΜΜΩΝ","ΣΥΣΧΕΤΙΣΜΟΣ ΥΔΡΟΓΡΑΦΙΚΩΝ ΣΥΣΤΗΜΑΤΩΝ","ΥΔΡΟΓΡΑΦΙΚΑ ΣΥΣΤΗΜΑΤΑ","AZIMUTHS OF STREAM SEGMENTS-FAULT LINEAMENTS","Drainage systems","Factor analysis","Palaeogeographical evolution","VOLVI MOUNTAINS-NORTH GREECE"]}]},{"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/1531","http://hdl.handle.net/10442/hedi/1531"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["THE AIM OF THE THESIS WAS THE DETECTION OF THE POSSIBLE STAGES OF THE DEVELOPMENT AND EVOLUTION OF THE DRAINAGE SYSTEMS ON VOLVI MOUNTAINS. THE DRAINAGE SYSTEMS WERE DRAWN FROM AIRPHOTOS AND WERE USED TO MEASURE AND CALCULATE PARAMETERS WHICH EXPRESS THE DIMENSION AND SHAPE OF THE BASINS, THE RELIEF, THE DEGREE OF DISSECTION AND THE AZIMUTHS OF THE STREAM SEGMENTS. THESE AZIMUTHS SHOWED HOW MUCH THE DRAINAGE NETWORK WAS INFLUENCED BY THE FAULT LINES. THE REST OF THE PARAMETERS STUDIED BY FACTOR ANALYSIS AND GAVE NEW EVIDENCES CONCERNING THE ROLE OF THE BASIN RELIEF ON THE FORMATION OF THE BASIN'S DIMENSIONS. ALSO, THREE ISOLINE MAPS WERE CONSTRUCTED PRESENTING THE EVOLUTION AND DEVELOPMENT OF THE DRAINAGE SYSTEMS AND PALAEORELIEF IN TWO SUCCESSIVELY STAGES.","ΣΚΟΠΟΣ ΤΗΣ ΔΙΑΤΡΙΒΗΣ ΗΤΑΝ Ο ΕΝΤΟΠΙΣΜΟΣ ΤΩΝ ΣΤΑΔΙΩΝ ΑΝΑΠΤΥΞΗΣ ΚΑΙ ΤΟΥ ΤΡΟΠΟΥ ΕΞΕΛΙΞΗΣ ΤΩΝ ΥΔΡΟΓΡΑΦΙΚΩΝ ΣΥΣΤΗΜΑΤΩΝ ΠΟΥ ΑΝΑΠΤΥΣΣΟΝΤΑΙ ΣΤΑ ΟΡΗ ΤΗΣ ΒΟΛΒΗΣ. ΤΑ ΥΔΡΟΓΡΑΦΙΚΑ ΣΥΣΤΗΜΑΤΑ ΤΗΣ ΠΕΡΙΟΧΗΣ ΜΕΛΕΤΗΣ ΑΠΟΤΥΠΩΘΗΚΑΝ ΑΠΟ ΑΕΡΟΦΩΤΟΓΡΑΦΙΕΣ ΚΑΙ ΜΕΤΡΗΘΗΚΑΝ ΣΕ ΑΥΤΑ ΠΑΡΑΜΕΤΡΟΙ ΠΟΥ ΣΥΝΔΕΟΝΤΑΙ ΜΕ ΤΙΣ ΔΙΑΣΤΑΣΕΙΣ, ΤΟ ΣΧΗΜΑ, ΤΟ ΑΝΑΓΛΥΦΟ, ΤΟ ΒΑΘΜΟ ΔΙΑΜΕΛΙΣΜΟΥ ΚΑΙ ΤΗ ΔΙΕΥΘΥΝΣΗ ΡΟΗΣ ΤΟΥ ΔΙΚΤΥΟΥ (ΑΖΙΜΟΥΘΙΟ ΤΩΝ ΚΟΙΤΩΝ). ΤΑ ΑΖΙΜΟΥΘΙΑ ΤΩΝ ΚΟΙΤΩΝ ΦΑΝΕΡΩΣΑΝ ΤΟΝ ΒΑΘΜΟ ΕΞΑΡΤΗΣΗΣ ΤΟΥ ΔΙΚΤΥΟΥ ΑΠΟ ΤΗΝ ΤΕΚΤΟΝΙΚΗ ΤΗΣ ΠΕΡΙΟΧΗΣ. ΟΙ ΥΠΟΛΟΙΠΕΣ ΠΑΡΑΜΕΤΡΟΙ ΕΠΕΞΕΡΓΑΣΤΗΚΑΝ ΣΤΑΤΙΣΤΙΚΑ ΜΕ ΤΗΝ ΜΕΘΟΔΟ ΤΗΣ ΠΑΡΑΓΟΝΤΙΚΗΣ ΑΝΑΛΥΣΗΣ ΚΑΙ ΠΡΟΕΚΥΨΑΝ ΝΕΑ ΣΤΟΙΧΕΙΑ ΓΙΑ ΤΟ ΡΟΛΟ ΤΟΥ ΤΟΠΙΚΟΥ ΑΝΑΓΛΥΦΟΥ ΣΤΗ ΔΙΑΜΟΡΦΩΣΗ ΤΩΝ ΔΙΑΣΤΑΣΕΩΝ ΤΩΝ ΛΕΚΑΝΩΝ ΑΠΟΡΡΟΗΣ, ΚΑΘΩΣ ΚΑΙΤΡΕΙΣ ΧΑΡΤΕΣ ΙΣΑΡΙΘΜΗΤΙΚΩΝ ΚΑΜΠΥΛΩΝ ΠΟΥ ΠΑΡΟΥΣΙΑΖΟΥΝ ΣΕ ΔΥΟ ΧΡΟΝΙΚΑ ΣΤΑΔΙΑ ΤΗΝΕΞΕΛΙΞΗ ΤΩΝ ΥΔΡΟΓΡΑΦΙΚΩΝ ΣΥΣΤΗΜΑΤΩΝ ΚΑΙ ΤΟΥ ΠΑΛΑΙΟΑΝΑΓΛΥΦΟΥ ΣΤΗΝ ΠΕΡΙΟΧΗ."]},{"key":"dc:title","label":"Title","values":["ΣΥΜΒΟΛΗ ΤΗΣ ΠΟΣΟΤΙΚΗΣ ΜΕΛΕΤΗΣ ΤΩΝ ΥΔΡΟΓΡΑΦΙΚΩΝ ΣΥΣΤΗΜΑΤΩΝ ΣΤΗΝ ΠΑΛΑΙΟΓΕΩΓΡΑΦΙΚΗ ΕΞΕΛΙΞΗ ΤΩΝ ΟΡΕΩΝ ΤΗΣ ΒΟΛΒΗΣ","A CONTRIBUTION TO QUANTITATIVE STUDY OF DRAINAGE SYSTEMS IN PALEOGEOGRAPHICAL EVOLUTION OF VOLVI MOUNTAINS CENTRAL MACEDONIA NORTH GREECE"]}]}],"canonical_facts":{"dc:creator":["Λαμπρινός, Νικόλαος","Lambrinos, Nikolaos"],"dc:date":["1989"],"dc:description":["THE AIM OF THE THESIS WAS THE DETECTION OF THE POSSIBLE STAGES OF THE DEVELOPMENT AND EVOLUTION OF THE DRAINAGE SYSTEMS ON VOLVI MOUNTAINS. THE DRAINAGE SYSTEMS WERE DRAWN FROM AIRPHOTOS AND WERE USED TO MEASURE AND CALCULATE PARAMETERS WHICH EXPRESS THE DIMENSION AND SHAPE OF THE BASINS, THE RELIEF, THE DEGREE OF DISSECTION AND THE AZIMUTHS OF THE STREAM SEGMENTS. THESE AZIMUTHS SHOWED HOW MUCH THE DRAINAGE NETWORK WAS INFLUENCED BY THE FAULT LINES. THE REST OF THE PARAMETERS STUDIED BY FACTOR ANALYSIS AND GAVE NEW EVIDENCES CONCERNING THE ROLE OF THE BASIN RELIEF ON THE FORMATION OF THE BASIN'S DIMENSIONS. ALSO, THREE ISOLINE MAPS WERE CONSTRUCTED PRESENTING THE EVOLUTION AND DEVELOPMENT OF THE DRAINAGE SYSTEMS AND PALAEORELIEF IN TWO SUCCESSIVELY STAGES.","ΣΚΟΠΟΣ ΤΗΣ ΔΙΑΤΡΙΒΗΣ ΗΤΑΝ Ο ΕΝΤΟΠΙΣΜΟΣ ΤΩΝ ΣΤΑΔΙΩΝ ΑΝΑΠΤΥΞΗΣ ΚΑΙ ΤΟΥ ΤΡΟΠΟΥ ΕΞΕΛΙΞΗΣ ΤΩΝ ΥΔΡΟΓΡΑΦΙΚΩΝ ΣΥΣΤΗΜΑΤΩΝ ΠΟΥ ΑΝΑΠΤΥΣΣΟΝΤΑΙ ΣΤΑ ΟΡΗ ΤΗΣ ΒΟΛΒΗΣ. ΤΑ ΥΔΡΟΓΡΑΦΙΚΑ ΣΥΣΤΗΜΑΤΑ ΤΗΣ ΠΕΡΙΟΧΗΣ ΜΕΛΕΤΗΣ ΑΠΟΤΥΠΩΘΗΚΑΝ ΑΠΟ ΑΕΡΟΦΩΤΟΓΡΑΦΙΕΣ ΚΑΙ ΜΕΤΡΗΘΗΚΑΝ ΣΕ ΑΥΤΑ ΠΑΡΑΜΕΤΡΟΙ ΠΟΥ ΣΥΝΔΕΟΝΤΑΙ ΜΕ ΤΙΣ ΔΙΑΣΤΑΣΕΙΣ, ΤΟ ΣΧΗΜΑ, ΤΟ ΑΝΑΓΛΥΦΟ, ΤΟ ΒΑΘΜΟ ΔΙΑΜΕΛΙΣΜΟΥ ΚΑΙ ΤΗ ΔΙΕΥΘΥΝΣΗ ΡΟΗΣ ΤΟΥ ΔΙΚΤΥΟΥ (ΑΖΙΜΟΥΘΙΟ ΤΩΝ ΚΟΙΤΩΝ). ΤΑ ΑΖΙΜΟΥΘΙΑ ΤΩΝ ΚΟΙΤΩΝ ΦΑΝΕΡΩΣΑΝ ΤΟΝ ΒΑΘΜΟ ΕΞΑΡΤΗΣΗΣ ΤΟΥ ΔΙΚΤΥΟΥ ΑΠΟ ΤΗΝ ΤΕΚΤΟΝΙΚΗ ΤΗΣ ΠΕΡΙΟΧΗΣ. ΟΙ ΥΠΟΛΟΙΠΕΣ ΠΑΡΑΜΕΤΡΟΙ ΕΠΕΞΕΡΓΑΣΤΗΚΑΝ ΣΤΑΤΙΣΤΙΚΑ ΜΕ ΤΗΝ ΜΕΘΟΔΟ ΤΗΣ ΠΑΡΑΓΟΝΤΙΚΗΣ ΑΝΑΛΥΣΗΣ ΚΑΙ ΠΡΟΕΚΥΨΑΝ ΝΕΑ ΣΤΟΙΧΕΙΑ ΓΙΑ ΤΟ ΡΟΛΟ ΤΟΥ ΤΟΠΙΚΟΥ ΑΝΑΓΛΥΦΟΥ ΣΤΗ ΔΙΑΜΟΡΦΩΣΗ ΤΩΝ ΔΙΑΣΤΑΣΕΩΝ ΤΩΝ ΛΕΚΑΝΩΝ ΑΠΟΡΡΟΗΣ, ΚΑΘΩΣ ΚΑΙΤΡΕΙΣ ΧΑΡΤΕΣ ΙΣΑΡΙΘΜΗΤΙΚΩΝ ΚΑΜΠΥΛΩΝ ΠΟΥ ΠΑΡΟΥΣΙΑΖΟΥΝ ΣΕ ΔΥΟ ΧΡΟΝΙΚΑ ΣΤΑΔΙΑ ΤΗΝΕΞΕΛΙΞΗ ΤΩΝ ΥΔΡΟΓΡΑΦΙΚΩΝ ΣΥΣΤΗΜΑΤΩΝ ΚΑΙ ΤΟΥ ΠΑΛΑΙΟΑΝΑΓΛΥΦΟΥ ΣΤΗΝ ΠΕΡΙΟΧΗ."],"dc:identifier":["10.12681/eadd/1531","http://hdl.handle.net/10442/hedi/1531"],"dc:language":["gre"],"dc:publisher":["Aristotle University Of Thessaloniki (AUTH)","Αριστοτέλειο Πανεπιστήμιο Θεσσαλονίκης (ΑΠΘ)"],"dc:subject":["ΜΗ ΠΑΡΑΜΕΤΡΙΚΗ ΣΤΑΤΙΣΤΙΚΗ","Παλαιογεωγραφική εξέλιξη","Παραγοντική ανάλυση","ΣΥΣΧΕΤΙΣΜΟΣ ΤΕΚΤΟΝΙΚΩΝ ΓΡΑΜΜΩΝ","ΣΥΣΧΕΤΙΣΜΟΣ ΥΔΡΟΓΡΑΦΙΚΩΝ ΣΥΣΤΗΜΑΤΩΝ","ΥΔΡΟΓΡΑΦΙΚΑ ΣΥΣΤΗΜΑΤΑ","AZIMUTHS OF STREAM SEGMENTS-FAULT LINEAMENTS","Drainage systems","Factor analysis","Palaeogeographical evolution","VOLVI MOUNTAINS-NORTH GREECE"],"dc:title":["ΣΥΜΒΟΛΗ ΤΗΣ ΠΟΣΟΤΙΚΗΣ ΜΕΛΕΤΗΣ ΤΩΝ ΥΔΡΟΓΡΑΦΙΚΩΝ ΣΥΣΤΗΜΑΤΩΝ ΣΤΗΝ ΠΑΛΑΙΟΓΕΩΓΡΑΦΙΚΗ ΕΞΕΛΙΞΗ ΤΩΝ ΟΡΕΩΝ ΤΗΣ ΒΟΛΒΗΣ","A CONTRIBUTION TO QUANTITATIVE STUDY OF DRAINAGE SYSTEMS IN PALEOGEOGRAPHICAL EVOLUTION OF VOLVI MOUNTAINS CENTRAL MACEDONIA NORTH GREECE"],"dc:type":["PhD Thesis"]},"updated_at":"2026-07-24T02:24:59Z"}