{"id":{"repo_id":"greece","oai_identifier":"oai:10442/0634"},"canonical_url":"https://search.dev.ndltd.org/etd/greece/oai:10442/0634","repository":{"repo_id":"greece","name":"Greek National Archive of PhD Theses","base_url":"https://phdtheses.ekt.gr/eadd_oai/request"},"display":{"title":"ΓΕΩΛΟΓΙΚΗ ΔΟΜΗ ΚΑΙ ΓΕΩΔΥΝΑΜΙΚΗ ΕΞΕΛΙΞΗ ΤΗΣ ΟΡΟΣΕΙΡΑΣ ΤΟΥ ΚΟΖΙΑΚΑ (ΔΥΤΙΚΗ ΘΕΣΣΑΛΙΑ)","abstract":"THE OBJECT OF EXAMINATION IS THE GEOLOGICAL STRUCTURE OF THE KOZAKAS RANGE, WHICH IS CONSTRUCTED MAINLY BY FORMATIONS OF THE WESTERN THESSALY UNIT, AGED UPPERTRIASSIC-MIDDLE-UPPER EOCENE. AFTER STUDIES ON THE LITHOSTRATIGRAPHY TECTONIC,STRUCTURE AND DEFORMATION, THERE HAS BEEN CONFIRMED THAT DURING THE IURASSIC PERIOD WAS THE MAIN AREAS OF SEDIMENTATION WERE A) A PLATFORM WITH HERITIC SEDIMENTATION B) A SLOPE BY THE PLATFORM WITH PELAGIC- ABYSIAL SEDIMENTS AND OPHIOLITES. THE REPRESENTATION OF THE PALAEOGEOGRAPHY OF THE UNIT'S REGION LED TO ITS POSITIONING IN THE TETHYS SYSTEM.","abstract_html":"THE OBJECT OF EXAMINATION IS THE GEOLOGICAL STRUCTURE OF THE KOZAKAS RANGE, WHICH IS CONSTRUCTED MAINLY BY FORMATIONS OF THE WESTERN THESSALY UNIT, AGED UPPERTRIASSIC-MIDDLE-UPPER EOCENE. AFTER STUDIES ON THE LITHOSTRATIGRAPHY TECTONIC,STRUCTURE AND DEFORMATION, THERE HAS BEEN CONFIRMED THAT DURING THE IURASSIC PERIOD WAS THE MAIN AREAS OF SEDIMENTATION WERE A) A PLATFORM WITH HERITIC SEDIMENTATION B) A SLOPE BY THE PLATFORM WITH PELAGIC- ABYSIAL SEDIMENTS AND OPHIOLITES. THE REPRESENTATION OF THE PALAEOGEOGRAPHY OF THE UNIT'S REGION LED TO ITS POSITIONING IN THE TETHYS SYSTEM.","abstract_has_math":false,"creators":["Λέκκας, Ευθύμιος","Lekkas, Efthymios"],"institution":"National and Kapodistrian University of Athens","degree_name":null,"degree_level":null,"degree_discipline":null,"degree_department":null,"school":null,"contributors":[],"advisors":[],"committee_chairs":[],"committee_members":[],"year":1988,"date_issued":"1988","date_published":"1988","updated_at":"2026-07-24T02:25:24Z","subjects":["Γεωδυναμική εξέλιξη","Γεωλογική δομή","Ελλάδα","Θεσσαλία","Κόζιακας","ΛΙΘΟΣΤΡΩΜΑΤΟΓΡΑΦΙΚΗ ΔΙΑΡΘΡΩΣΗ","Οφιόλιθοι","ΤΕΚΤΟΝΙΚΗ ΔΟΜΗ-ΠΑΡΑΜΟΡΦΩΣΗ","ΩΚΕΑΝΟΣ ΔΥΤΙΚΗΣ ΘΕΣΣΑΛΙΑΣ","Geodynamic evolution","Geological structure","Hellas","Koziakas","LITHOSTRATIGRAPHY STRUCTURE","OFIOLITE","TECTONIC STRUCTURE","Thessaly","WEST THESSALY BASIN"],"languages":["gre"],"rights":[],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier","label":"Identifier","values":["10.12681/eadd/0634"],"render_values":[{"text":"10.12681/eadd/0634","href":"https://doi.org/10.12681/eadd/0634","code":true}]}]},"links":{"outbound_url":"http://hdl.handle.net/10442/hedi/0634","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:creator","label":"Author","values":["Λέκκας, Ευθύμιος","Lekkas, Efthymios"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["1988"]},{"key":"dc:publisher","label":"Institution","values":["National and Kapodistrian University of Athens","Εθνικό και Καποδιστριακό Πανεπιστήμιο Αθηνών (ΕΚΠΑ)"]},{"key":"dc:type","label":"Dc Type","values":["PhD Thesis"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["Γεωδυναμική εξέλιξη","Γεωλογική δομή","Ελλάδα","Θεσσαλία","Κόζιακας","ΛΙΘΟΣΤΡΩΜΑΤΟΓΡΑΦΙΚΗ ΔΙΑΡΘΡΩΣΗ","Οφιόλιθοι","ΤΕΚΤΟΝΙΚΗ ΔΟΜΗ-ΠΑΡΑΜΟΡΦΩΣΗ","ΩΚΕΑΝΟΣ ΔΥΤΙΚΗΣ ΘΕΣΣΑΛΙΑΣ","Geodynamic evolution","Geological structure","Hellas","Koziakas","LITHOSTRATIGRAPHY STRUCTURE","OFIOLITE","TECTONIC STRUCTURE","Thessaly","WEST THESSALY BASIN"]}]},{"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/0634","http://hdl.handle.net/10442/hedi/0634"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["THE OBJECT OF EXAMINATION IS THE GEOLOGICAL STRUCTURE OF THE KOZAKAS RANGE, WHICH IS CONSTRUCTED MAINLY BY FORMATIONS OF THE WESTERN THESSALY UNIT, AGED UPPERTRIASSIC-MIDDLE-UPPER EOCENE. AFTER STUDIES ON THE LITHOSTRATIGRAPHY TECTONIC,STRUCTURE AND DEFORMATION, THERE HAS BEEN CONFIRMED THAT DURING THE IURASSIC PERIOD WAS THE MAIN AREAS OF SEDIMENTATION WERE A) A PLATFORM WITH HERITIC SEDIMENTATION B) A SLOPE BY THE PLATFORM WITH PELAGIC- ABYSIAL SEDIMENTS AND OPHIOLITES. THE REPRESENTATION OF THE PALAEOGEOGRAPHY OF THE UNIT'S REGION LED TO ITS POSITIONING IN THE TETHYS SYSTEM.","ΕΞΕΤΑΖΕΤΑΙ Η ΓΕΩΛΟΓΙΚΗ ΔΟΜΗ ΤΗΣ ΟΡΟΣΕΙΡΑΣ ΤΟΥ ΚΥΤΙΑΚΑ (ΔΥΤΙΚΗ ΘΕΣΣΑΛΙΑ, ΕΛΛΑΔΑ)Η ΟΠΟΙΑ ΔΟΜΕΙΤΑΙ ΑΠΟ ΣΧΗΜΑΤΙΣΜΟΥΣ ΤΗΣ ΕΝΟΤΗΤΑΣ ΔΥΤΙΚΗΣ ΘΕΣΣΑΛΙΑΣ ΗΛΙΚΙΑΣ ΑΝΩΤΕΡΟΥ ΤΡΙΑΔΙΚΟΥ-ΜΕΣΟΥ ΑΝΩΤΕΡΟΥ ΗΩΚΑΙΝΟΥ. ΜΕΤΑ ΑΠΟ ΛΙΘΟΣΤΡΩΜΑΤΟΓΡΑΦΙΚΗ ΜΕΛΕΤΗ, ΜΕΛΕΤΗ ΤΗΣ ΤΕΚΤΟΝΙΚΗΣ ΔΟΜΗΣ ΠΑΡΑΜΟΡΦΩΣΗΣ ΔΙΑΠΙΣΤΩΘΗΚΕ ΟΤΙ ΚΑΤΑ ΤΗ ΔΙΑΡΚΕΙΑ ΤΟΥ ΙΟΥΡΑΣΙΚΟΥ ΛΕΙΤΟΥΡΓΗΣΕ ΣΤΟ ΧΩΡΟ ΤΗΣ ΕΝΟΤΗΤΑΣ ΔΥΤΙΚΗΣ ΘΕΣΣΑΛΙΑΣ (Α) ΜΙΑ ΤΡΑΠΕΖΑ ΜΕ ΝΗΡΙΤΙΚΗ ΙΖΗΜΑΤΟΓΕΝΕΣΗ (Β) ΜΙΑ ΚΛΙΤΥΣ ΔΙΠΛΑ ΣΤΗΝ ΤΡΑΠΕΖΑ ΜΕ ΑΠΟΘΕΣΕΙΣ ΧΑΡΑΚΤΗΡΙΣΤΙΚΩΝ ΣΧΗΜΑΤΙΣΜΩΝ ΚΛΙΤΥΩΝ ΚΑΙ (Γ) ΜΙΑ ΩΚΕΑΝΕΙΑ ΛΕΚΑΝΗ ΜΕ ΠΕΛΑΓΙΚΑ- ΑΒΥΣΣΙΚΑ ΙΖΗΜΑΤΑ ΚΑΙ ΟΦΙΟΛΙΘΟΥΣ. Η ΑΝΑΠΑΡΑΣΤΑΣΗ ΤΟΥ ΠΑΛΑΙΟΓΕΩΓΡΑΦΙΚΟΥ ΧΩΡΟΥ ΤΗΣ ΕΝΟΤΗΤΑΣ ΜΕ ΔΙΑΣΤΗΜΑ ΤΟΥ ΙΟΥΡΑΣΙΚΟΥ ΑΛΛΑ ΚΑΙ ΣΕ ΑΛΛΑ ΧΡΟΝΙΚΑ ΔΙΑΣΤΗΜΑΤΑ ΕΠΕΤΡΕΨΕ ΤΗΝ ΕΝΤΑΞΗ ΤΟΥ, ΣΤΗΝ ΟΡΓΑΝΩΣΗ ΤΗΣ ΤΗΘΥΟΣ."]},{"key":"dc:title","label":"Title","values":["ΓΕΩΛΟΓΙΚΗ ΔΟΜΗ ΚΑΙ ΓΕΩΔΥΝΑΜΙΚΗ ΕΞΕΛΙΞΗ ΤΗΣ ΟΡΟΣΕΙΡΑΣ ΤΟΥ ΚΟΖΙΑΚΑ (ΔΥΤΙΚΗ ΘΕΣΣΑΛΙΑ)","GEOLOGICAL STRUCTURE AND GEODYNAMIC EVOLUTION OF THE KOZIAKAS RANCE (WEST THESSALY)"]}]}],"canonical_facts":{"dc:creator":["Λέκκας, Ευθύμιος","Lekkas, Efthymios"],"dc:date":["1988"],"dc:description":["THE OBJECT OF EXAMINATION IS THE GEOLOGICAL STRUCTURE OF THE KOZAKAS RANGE, WHICH IS CONSTRUCTED MAINLY BY FORMATIONS OF THE WESTERN THESSALY UNIT, AGED UPPERTRIASSIC-MIDDLE-UPPER EOCENE. AFTER STUDIES ON THE LITHOSTRATIGRAPHY TECTONIC,STRUCTURE AND DEFORMATION, THERE HAS BEEN CONFIRMED THAT DURING THE IURASSIC PERIOD WAS THE MAIN AREAS OF SEDIMENTATION WERE A) A PLATFORM WITH HERITIC SEDIMENTATION B) A SLOPE BY THE PLATFORM WITH PELAGIC- ABYSIAL SEDIMENTS AND OPHIOLITES. THE REPRESENTATION OF THE PALAEOGEOGRAPHY OF THE UNIT'S REGION LED TO ITS POSITIONING IN THE TETHYS SYSTEM.","ΕΞΕΤΑΖΕΤΑΙ Η ΓΕΩΛΟΓΙΚΗ ΔΟΜΗ ΤΗΣ ΟΡΟΣΕΙΡΑΣ ΤΟΥ ΚΥΤΙΑΚΑ (ΔΥΤΙΚΗ ΘΕΣΣΑΛΙΑ, ΕΛΛΑΔΑ)Η ΟΠΟΙΑ ΔΟΜΕΙΤΑΙ ΑΠΟ ΣΧΗΜΑΤΙΣΜΟΥΣ ΤΗΣ ΕΝΟΤΗΤΑΣ ΔΥΤΙΚΗΣ ΘΕΣΣΑΛΙΑΣ ΗΛΙΚΙΑΣ ΑΝΩΤΕΡΟΥ ΤΡΙΑΔΙΚΟΥ-ΜΕΣΟΥ ΑΝΩΤΕΡΟΥ ΗΩΚΑΙΝΟΥ. ΜΕΤΑ ΑΠΟ ΛΙΘΟΣΤΡΩΜΑΤΟΓΡΑΦΙΚΗ ΜΕΛΕΤΗ, ΜΕΛΕΤΗ ΤΗΣ ΤΕΚΤΟΝΙΚΗΣ ΔΟΜΗΣ ΠΑΡΑΜΟΡΦΩΣΗΣ ΔΙΑΠΙΣΤΩΘΗΚΕ ΟΤΙ ΚΑΤΑ ΤΗ ΔΙΑΡΚΕΙΑ ΤΟΥ ΙΟΥΡΑΣΙΚΟΥ ΛΕΙΤΟΥΡΓΗΣΕ ΣΤΟ ΧΩΡΟ ΤΗΣ ΕΝΟΤΗΤΑΣ ΔΥΤΙΚΗΣ ΘΕΣΣΑΛΙΑΣ (Α) ΜΙΑ ΤΡΑΠΕΖΑ ΜΕ ΝΗΡΙΤΙΚΗ ΙΖΗΜΑΤΟΓΕΝΕΣΗ (Β) ΜΙΑ ΚΛΙΤΥΣ ΔΙΠΛΑ ΣΤΗΝ ΤΡΑΠΕΖΑ ΜΕ ΑΠΟΘΕΣΕΙΣ ΧΑΡΑΚΤΗΡΙΣΤΙΚΩΝ ΣΧΗΜΑΤΙΣΜΩΝ ΚΛΙΤΥΩΝ ΚΑΙ (Γ) ΜΙΑ ΩΚΕΑΝΕΙΑ ΛΕΚΑΝΗ ΜΕ ΠΕΛΑΓΙΚΑ- ΑΒΥΣΣΙΚΑ ΙΖΗΜΑΤΑ ΚΑΙ ΟΦΙΟΛΙΘΟΥΣ. Η ΑΝΑΠΑΡΑΣΤΑΣΗ ΤΟΥ ΠΑΛΑΙΟΓΕΩΓΡΑΦΙΚΟΥ ΧΩΡΟΥ ΤΗΣ ΕΝΟΤΗΤΑΣ ΜΕ ΔΙΑΣΤΗΜΑ ΤΟΥ ΙΟΥΡΑΣΙΚΟΥ ΑΛΛΑ ΚΑΙ ΣΕ ΑΛΛΑ ΧΡΟΝΙΚΑ ΔΙΑΣΤΗΜΑΤΑ ΕΠΕΤΡΕΨΕ ΤΗΝ ΕΝΤΑΞΗ ΤΟΥ, ΣΤΗΝ ΟΡΓΑΝΩΣΗ ΤΗΣ ΤΗΘΥΟΣ."],"dc:identifier":["10.12681/eadd/0634","http://hdl.handle.net/10442/hedi/0634"],"dc:language":["gre"],"dc:publisher":["National and Kapodistrian University of Athens","Εθνικό και Καποδιστριακό Πανεπιστήμιο Αθηνών (ΕΚΠΑ)"],"dc:subject":["Γεωδυναμική εξέλιξη","Γεωλογική δομή","Ελλάδα","Θεσσαλία","Κόζιακας","ΛΙΘΟΣΤΡΩΜΑΤΟΓΡΑΦΙΚΗ ΔΙΑΡΘΡΩΣΗ","Οφιόλιθοι","ΤΕΚΤΟΝΙΚΗ ΔΟΜΗ-ΠΑΡΑΜΟΡΦΩΣΗ","ΩΚΕΑΝΟΣ ΔΥΤΙΚΗΣ ΘΕΣΣΑΛΙΑΣ","Geodynamic evolution","Geological structure","Hellas","Koziakas","LITHOSTRATIGRAPHY STRUCTURE","OFIOLITE","TECTONIC STRUCTURE","Thessaly","WEST THESSALY BASIN"],"dc:title":["ΓΕΩΛΟΓΙΚΗ ΔΟΜΗ ΚΑΙ ΓΕΩΔΥΝΑΜΙΚΗ ΕΞΕΛΙΞΗ ΤΗΣ ΟΡΟΣΕΙΡΑΣ ΤΟΥ ΚΟΖΙΑΚΑ (ΔΥΤΙΚΗ ΘΕΣΣΑΛΙΑ)","GEOLOGICAL STRUCTURE AND GEODYNAMIC EVOLUTION OF THE KOZIAKAS RANCE (WEST THESSALY)"],"dc:type":["PhD Thesis"]},"updated_at":"2026-07-24T02:25:24Z"}