{"id":{"repo_id":"greece","oai_identifier":"oai:10442/1735"},"canonical_url":"https://search.dev.ndltd.org/etd/greece/oai:10442/1735","repository":{"repo_id":"greece","name":"Greek National Archive of PhD Theses","base_url":"https://phdtheses.ekt.gr/eadd_oai/request"},"display":{"title":"ΠΕΡΙΒΑΛΛΟΝΤΑ ΙΖΗΜΑΤΟΓΕΝΕΣΗΣ ΚΑΙ ΠΑΓΕΤΟΕΥΣΤΑΤΙΚΕΣ ΚΙΝΗΣΕΙΣ ΤΩΝ ΤΕΤΑΡΤΟΓΕΝΩΝ ΑΠΟΘΕΣΕΩΝ ΤΗΣ ΠΕΡΙΟΧΗΣ Ν. ΜΑΝΩΛΑΔΑΣ-ΛΕΧΑΙΝΩΝ","abstract":"THE STUDY OF THE SEDIMENTARY ENVIRONMENTS AND OF THE GLACIAL- EUSTATIC MOVEMENTOF THE QUARTERNARY DEPOSITS IN THE MANOLADHA- LECHEINA AREA HAVE GIVEN THE FOLLOWING CONCLUSIONS: 1. THE STUDIED SEDIMENTARY SEQUENCES WERE DEPOSITED LATER THAN MID- PLEISTOCENE AND NOT DURING UPPER PLIOCENE, AS IT WAS BELIEVED BEFORE THIS STUDY. 2. THE EXAMINED AREA CONSISTS OF 4 GEOMORPHOLOGICAL ENVIRONMENTS: A.MOUNTAIN FRONT; B. PIEDMONT; C. MARINE TERRACE; D. COASTAL PLAIN. THE MOUNTAINFRONT IS CONTROLLED BY A FAULT/EROSIONAL SURFACE AND IS CUT DOWN BY CANYONS WHOSE INCLINATION IS LESS THAN INCLINATION OF THE FRONT SURFACE. THE FAULT CONTROLLED SURFACE HAS NOT REACTIVATED AFTER THE DEVELOPMENT OF THE MARINE TERRACE. (SHORTENED)","abstract_html":"THE STUDY OF THE SEDIMENTARY ENVIRONMENTS AND OF THE GLACIAL- EUSTATIC MOVEMENTOF THE QUARTERNARY DEPOSITS IN THE MANOLADHA- LECHEINA AREA HAVE GIVEN THE FOLLOWING CONCLUSIONS: 1. THE STUDIED SEDIMENTARY SEQUENCES WERE DEPOSITED LATER THAN MID- PLEISTOCENE AND NOT DURING UPPER PLIOCENE, AS IT WAS BELIEVED BEFORE THIS STUDY. 2. THE EXAMINED AREA CONSISTS OF 4 GEOMORPHOLOGICAL ENVIRONMENTS: A.MOUNTAIN FRONT; B. PIEDMONT; C. MARINE TERRACE; D. COASTAL PLAIN. THE MOUNTAINFRONT IS CONTROLLED BY A FAULT/EROSIONAL SURFACE AND IS CUT DOWN BY CANYONS WHOSE INCLINATION IS LESS THAN INCLINATION OF THE FRONT SURFACE. THE FAULT CONTROLLED SURFACE HAS NOT REACTIVATED AFTER THE DEVELOPMENT OF THE MARINE TERRACE. (SHORTENED)","abstract_has_math":false,"creators":["Σταματόπουλος, Λεωνίδας"],"institution":"University of Patras","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":["ΛΕΧΑΙΝΑ","Ν. ΜΑΝΩΛΑΔΑ","ΠΑΓΕΤΟΕΥΣΤΑΤΙΚΕΣ ΚΙΝΗΣΕΙΣ","Περιβάλλοντα ιζηματογένεσης","Τεταρτογενείς αποθέσεις","GLACIAL-EUSTASTIC MOVEMENTS","LECHENA","N. MANOLADA","QUARTERNARY DEPOSITS","Sedimentary environments"],"languages":["gre"],"rights":[],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier","label":"Identifier","values":["10.12681/eadd/1735"],"render_values":[{"text":"10.12681/eadd/1735","href":"https://doi.org/10.12681/eadd/1735","code":true}]}]},"links":{"outbound_url":"http://hdl.handle.net/10442/hedi/1735","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:creator","label":"Author","values":["Σταματόπουλος, Λεωνίδας"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["1991"]},{"key":"dc:publisher","label":"Institution","values":["University of Patras","Πανεπιστήμιο Πατρών"]},{"key":"dc:type","label":"Dc Type","values":["PhD Thesis"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["ΛΕΧΑΙΝΑ","Ν. ΜΑΝΩΛΑΔΑ","ΠΑΓΕΤΟΕΥΣΤΑΤΙΚΕΣ ΚΙΝΗΣΕΙΣ","Περιβάλλοντα ιζηματογένεσης","Τεταρτογενείς αποθέσεις","GLACIAL-EUSTASTIC MOVEMENTS","LECHENA","N. MANOLADA","QUARTERNARY DEPOSITS","Sedimentary environments"]}]},{"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/1735","http://hdl.handle.net/10442/hedi/1735"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["THE STUDY OF THE SEDIMENTARY ENVIRONMENTS AND OF THE GLACIAL- EUSTATIC MOVEMENTOF THE QUARTERNARY DEPOSITS IN THE MANOLADHA- LECHEINA AREA HAVE GIVEN THE FOLLOWING CONCLUSIONS: 1. THE STUDIED SEDIMENTARY SEQUENCES WERE DEPOSITED LATER THAN MID- PLEISTOCENE AND NOT DURING UPPER PLIOCENE, AS IT WAS BELIEVED BEFORE THIS STUDY. 2. THE EXAMINED AREA CONSISTS OF 4 GEOMORPHOLOGICAL ENVIRONMENTS: A.MOUNTAIN FRONT; B. PIEDMONT; C. MARINE TERRACE; D. COASTAL PLAIN. THE MOUNTAINFRONT IS CONTROLLED BY A FAULT/EROSIONAL SURFACE AND IS CUT DOWN BY CANYONS WHOSE INCLINATION IS LESS THAN INCLINATION OF THE FRONT SURFACE. THE FAULT CONTROLLED SURFACE HAS NOT REACTIVATED AFTER THE DEVELOPMENT OF THE MARINE TERRACE. (SHORTENED)","Η ΜΕΛΕΤΗ ΤΩΝ ΠΕΡΙΒΑΛΛΟΝΤΩΝ ΙΖΗΜΑΤΟΓΕΝΕΣΗΣ ΚΑΙ ΤΩΝ ΠΑΓΕΤΟΕΥΣΤΑΤΙΚΩΝ ΚΙΝΗΣΕΩΝ ΤΩΝΤΕΤΑΡΤΟΓΕΝΩΝ ΑΠΟΘΕΣΕΩΝ ΤΗΣ ΠΕΡΙΟΧΗΣ Ν. ΜΑΝΩΛΑΔΑΣ-ΛΕΧΑΙΝΩΝ ΕΔΩΣΕ ΤΑ ΠΑΡΑΚΑΤΩ ΣΥΜΠΕΡΑΣΜΑΤΑ. 1. Η ΗΛΙΚΙΑ ΤΩΝ ΜΕΛΕΤΗΘΕΝΤΩΝ ΙΖΗΜΑΤΩΝ ΕΙΝΑΙ ΝΕΩΤΕΡΗ ΤΟΥ ΜΕΣΟΥ ΠΛΕΙΣΤΟΚΑΙΝΟΥ. Η ΜΕΧΡΙ ΤΩΡΑ ΕΠΙΚΡΑΤΟΥΣΑ ΑΠΟΨΗ ΗΤΑΝ ΟΤΙ ΤΑ ΙΖΗΜΑΤΑ ΑΥΤΑ ΑΝΗΚΑΝ ΣΤΟ ΑΝΩΤΕΡΟ ΠΛΕΙΟΚΑΙΝΟ. 2. ΤΟ ΑΝΑΓΛΥΦΟ ΤΗΣ ΥΠΟ ΕΡΕΥΝΑ ΠΕΡΙΟΧΗΣ ΣΥΓΚΡΟΤΕΙΤΑΙ ΑΠΟ 4 ΓΕΩΜΟΡΦΕΣ: Α. ΜΕΤΩΠΟ ΒΟΥΝΟΥ Β. ΠΕΤΡΟΠΡΟΠΟΔΑ Γ. ΘΑΛΑΣΣΙΑ ΑΝΑΒΑΘΜΙΔΑ Δ. ΠΑΡΑΚΤΙΟ ΠΕΔΙΟ. - ΤΟ ΜΕΤΩΠΟ ΒΟΥΝΟΥ ΔΙΑΜΟΡΦΩΝΕΤΑΙ ΑΠΟ ΡΗΞΙΓΕΝΗ, ΔΙΑΒΡΩΣΙΓΕΝΗ ΕΠΙΦΑΝΕΙΑ ΠΟΥ ΔΙΑΤΕΜΝΕΤΑΙ ΣΕ ΕΥΡΕΙΣ ΤΡΙΓΩΝΙΚΕΣ ΕΝΤΟΜΕΣ ΤΩΝ ΟΠΟΙΩΝ ΟΙ ΚΛΙΣΕΙΣ ΕΙΝΑΙ ΜΙΚΡΟΤΕΡΕΣ ΤΗΣ ΔΙΑΡΡΗΞΗΣ. Η ΕΠΙΦΑΝΕΙΑ ΑΥΤΗ ΔΕΝ ΦΑΙΝΕΤΑΙ ΝΑ ΕΧΕΙ ΕΠΑΝΑΔΡΑΣΤΗΡΙΟΠΟΙΗΘΕΙ ΜΕΤΑΤΗΝ ΔΗΜΙΟΥΡΓΙΑ ΤΗΣ ΑΝΑΒΑΘΜΙΔΑΣ. (ΠΕΡΙΚΟΠΗ)"]},{"key":"dc:title","label":"Title","values":["ΠΕΡΙΒΑΛΛΟΝΤΑ ΙΖΗΜΑΤΟΓΕΝΕΣΗΣ ΚΑΙ ΠΑΓΕΤΟΕΥΣΤΑΤΙΚΕΣ ΚΙΝΗΣΕΙΣ ΤΩΝ ΤΕΤΑΡΤΟΓΕΝΩΝ ΑΠΟΘΕΣΕΩΝ ΤΗΣ ΠΕΡΙΟΧΗΣ Ν. ΜΑΝΩΛΑΔΑΣ-ΛΕΧΑΙΝΩΝ","THE SEDIMENTARY ENVIRONMENTS AND THE GLACIALEUSTATIC MOVEMENTS OF THE QUARTERNARY DEPOSITS IN THE N. MANOLADHA-LECHENA AREA"]}]}],"canonical_facts":{"dc:creator":["Σταματόπουλος, Λεωνίδας"],"dc:date":["1991"],"dc:description":["THE STUDY OF THE SEDIMENTARY ENVIRONMENTS AND OF THE GLACIAL- EUSTATIC MOVEMENTOF THE QUARTERNARY DEPOSITS IN THE MANOLADHA- LECHEINA AREA HAVE GIVEN THE FOLLOWING CONCLUSIONS: 1. THE STUDIED SEDIMENTARY SEQUENCES WERE DEPOSITED LATER THAN MID- PLEISTOCENE AND NOT DURING UPPER PLIOCENE, AS IT WAS BELIEVED BEFORE THIS STUDY. 2. THE EXAMINED AREA CONSISTS OF 4 GEOMORPHOLOGICAL ENVIRONMENTS: A.MOUNTAIN FRONT; B. PIEDMONT; C. MARINE TERRACE; D. COASTAL PLAIN. THE MOUNTAINFRONT IS CONTROLLED BY A FAULT/EROSIONAL SURFACE AND IS CUT DOWN BY CANYONS WHOSE INCLINATION IS LESS THAN INCLINATION OF THE FRONT SURFACE. THE FAULT CONTROLLED SURFACE HAS NOT REACTIVATED AFTER THE DEVELOPMENT OF THE MARINE TERRACE. (SHORTENED)","Η ΜΕΛΕΤΗ ΤΩΝ ΠΕΡΙΒΑΛΛΟΝΤΩΝ ΙΖΗΜΑΤΟΓΕΝΕΣΗΣ ΚΑΙ ΤΩΝ ΠΑΓΕΤΟΕΥΣΤΑΤΙΚΩΝ ΚΙΝΗΣΕΩΝ ΤΩΝΤΕΤΑΡΤΟΓΕΝΩΝ ΑΠΟΘΕΣΕΩΝ ΤΗΣ ΠΕΡΙΟΧΗΣ Ν. ΜΑΝΩΛΑΔΑΣ-ΛΕΧΑΙΝΩΝ ΕΔΩΣΕ ΤΑ ΠΑΡΑΚΑΤΩ ΣΥΜΠΕΡΑΣΜΑΤΑ. 1. Η ΗΛΙΚΙΑ ΤΩΝ ΜΕΛΕΤΗΘΕΝΤΩΝ ΙΖΗΜΑΤΩΝ ΕΙΝΑΙ ΝΕΩΤΕΡΗ ΤΟΥ ΜΕΣΟΥ ΠΛΕΙΣΤΟΚΑΙΝΟΥ. Η ΜΕΧΡΙ ΤΩΡΑ ΕΠΙΚΡΑΤΟΥΣΑ ΑΠΟΨΗ ΗΤΑΝ ΟΤΙ ΤΑ ΙΖΗΜΑΤΑ ΑΥΤΑ ΑΝΗΚΑΝ ΣΤΟ ΑΝΩΤΕΡΟ ΠΛΕΙΟΚΑΙΝΟ. 2. ΤΟ ΑΝΑΓΛΥΦΟ ΤΗΣ ΥΠΟ ΕΡΕΥΝΑ ΠΕΡΙΟΧΗΣ ΣΥΓΚΡΟΤΕΙΤΑΙ ΑΠΟ 4 ΓΕΩΜΟΡΦΕΣ: Α. ΜΕΤΩΠΟ ΒΟΥΝΟΥ Β. ΠΕΤΡΟΠΡΟΠΟΔΑ Γ. ΘΑΛΑΣΣΙΑ ΑΝΑΒΑΘΜΙΔΑ Δ. ΠΑΡΑΚΤΙΟ ΠΕΔΙΟ. - ΤΟ ΜΕΤΩΠΟ ΒΟΥΝΟΥ ΔΙΑΜΟΡΦΩΝΕΤΑΙ ΑΠΟ ΡΗΞΙΓΕΝΗ, ΔΙΑΒΡΩΣΙΓΕΝΗ ΕΠΙΦΑΝΕΙΑ ΠΟΥ ΔΙΑΤΕΜΝΕΤΑΙ ΣΕ ΕΥΡΕΙΣ ΤΡΙΓΩΝΙΚΕΣ ΕΝΤΟΜΕΣ ΤΩΝ ΟΠΟΙΩΝ ΟΙ ΚΛΙΣΕΙΣ ΕΙΝΑΙ ΜΙΚΡΟΤΕΡΕΣ ΤΗΣ ΔΙΑΡΡΗΞΗΣ. Η ΕΠΙΦΑΝΕΙΑ ΑΥΤΗ ΔΕΝ ΦΑΙΝΕΤΑΙ ΝΑ ΕΧΕΙ ΕΠΑΝΑΔΡΑΣΤΗΡΙΟΠΟΙΗΘΕΙ ΜΕΤΑΤΗΝ ΔΗΜΙΟΥΡΓΙΑ ΤΗΣ ΑΝΑΒΑΘΜΙΔΑΣ. (ΠΕΡΙΚΟΠΗ)"],"dc:identifier":["10.12681/eadd/1735","http://hdl.handle.net/10442/hedi/1735"],"dc:language":["gre"],"dc:publisher":["University of Patras","Πανεπιστήμιο Πατρών"],"dc:subject":["ΛΕΧΑΙΝΑ","Ν. ΜΑΝΩΛΑΔΑ","ΠΑΓΕΤΟΕΥΣΤΑΤΙΚΕΣ ΚΙΝΗΣΕΙΣ","Περιβάλλοντα ιζηματογένεσης","Τεταρτογενείς αποθέσεις","GLACIAL-EUSTASTIC MOVEMENTS","LECHENA","N. MANOLADA","QUARTERNARY DEPOSITS","Sedimentary environments"],"dc:title":["ΠΕΡΙΒΑΛΛΟΝΤΑ ΙΖΗΜΑΤΟΓΕΝΕΣΗΣ ΚΑΙ ΠΑΓΕΤΟΕΥΣΤΑΤΙΚΕΣ ΚΙΝΗΣΕΙΣ ΤΩΝ ΤΕΤΑΡΤΟΓΕΝΩΝ ΑΠΟΘΕΣΕΩΝ ΤΗΣ ΠΕΡΙΟΧΗΣ Ν. ΜΑΝΩΛΑΔΑΣ-ΛΕΧΑΙΝΩΝ","THE SEDIMENTARY ENVIRONMENTS AND THE GLACIALEUSTATIC MOVEMENTS OF THE QUARTERNARY DEPOSITS IN THE N. MANOLADHA-LECHENA AREA"],"dc:type":["PhD Thesis"]},"updated_at":"2026-07-24T02:25:05Z"}