{"id":{"repo_id":"greece","oai_identifier":"oai:10442/1400"},"canonical_url":"https://search.dev.ndltd.org/etd/greece/oai:10442/1400","repository":{"repo_id":"greece","name":"Greek National Archive of PhD Theses","base_url":"https://phdtheses.ekt.gr/eadd_oai/request"},"display":{"title":"ΤΕΚΤΟΝΙΚΕΣ ΚΙΝΗΣΕΙΣ ΚΑΤΑ ΤΟ ΤΕΤΑΡΤΟΓΕΝΕΣ ΣΤΙΣ ΑΚΤΕΣ ΤΗΣ ΑΝΑΤΟΛΙΚΗΣ ΚΡΗΤΗΣ","abstract":"THE SYSTEMATIC STUDY OF QUATERNARY MARINE PLATFORMS, PLEISTOCENE TERRACES, FAULTS, BEACH-ROCKS, HOLOCENE SHORELINES AND NEARSHORE ARCHAEOLOGICAL REMAINS AND FOUNDINGS ALLOWED US TO DETERMINE THE DIRECTION AND MAGNITUDE OF THE VERTICAL TECTONIC MOVEMENTS AND TECTONIC DEFORMATIONS THAT THE COASTS OF CENTRAL AND EASTERN PART OF CRETE ISLAND HAVE BEEN AFFECTED DURING QUATERNARY AND TO ARRIVE INTOCONCLUSIONS CONTRIBUTING TO THE RECENT GEOLOGICAL EVOLUTION OF THE ISLAND. (SHORTENED)","abstract_html":"THE SYSTEMATIC STUDY OF QUATERNARY MARINE PLATFORMS, PLEISTOCENE TERRACES, FAULTS, BEACH-ROCKS, HOLOCENE SHORELINES AND NEARSHORE ARCHAEOLOGICAL REMAINS AND FOUNDINGS ALLOWED US TO DETERMINE THE DIRECTION AND MAGNITUDE OF THE VERTICAL TECTONIC MOVEMENTS AND TECTONIC DEFORMATIONS THAT THE COASTS OF CENTRAL AND EASTERN PART OF CRETE ISLAND HAVE BEEN AFFECTED DURING QUATERNARY AND TO ARRIVE INTOCONCLUSIONS CONTRIBUTING TO THE RECENT GEOLOGICAL EVOLUTION OF THE ISLAND. (SHORTENED)","abstract_has_math":false,"creators":["Μουρτζάς, Νικόλαος"],"institution":"Εθνικό Μετσόβιο Πολυτεχνείο (ΕΜΠ)","degree_name":null,"degree_level":null,"degree_discipline":null,"degree_department":null,"school":null,"contributors":[],"advisors":[],"committee_chairs":[],"committee_members":[],"year":1990,"date_issued":"1990","date_published":"1990","updated_at":"2026-07-24T02:24:52Z","subjects":["Beach rocks","CRETE ISLAND","Faults","PLATFORMS","QUATERNARY","SHORELINES","TECTONIC BLOCKS","TECTONIC DEFORMATION","TERRACES","VERTICAL TECTONIC MOVEMENTS","ΑΚΤΟΓΡΑΜΜΕΣ","ΑΝΑΒΑΘΜΙΔΕΣ","ΕΠΙΦΑΝΕΙΕΣ ΙΣΟΠΕΔΩΣΗΣ","ΚΑΤΑΚΟΡΥΦΕΣ ΤΕΚΤΟΝΙΚΕΣ ΚΙΝΗΣΕΙΣ","Κρήτη","Ρήγματα","ΤΕΚΤΟΝΙΚΑ ΤΕΜΑΧΗ","ΤΕΚΤΟΝΙΚΕΣ ΠΑΡΑΜΟΡΦΩΣΕΙΣ","ΤΕΤΑΡΤΟΓΕΝΕΣ","Engineering and Technology","Environmental Engineering","Επιστήμες Μηχανικού και Τεχνολογία","Περιβαλλοντική Μηχανική"],"languages":["gre"],"rights":[],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier","label":"Identifier","values":["10.12681/eadd/1400"],"render_values":[{"text":"10.12681/eadd/1400","href":"https://doi.org/10.12681/eadd/1400","code":true}]}]},"links":{"outbound_url":"http://hdl.handle.net/10442/hedi/1400","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:creator","label":"Author","values":["Μουρτζάς, Νικόλαος"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["1990"]},{"key":"dc:publisher","label":"Institution","values":["Εθνικό Μετσόβιο Πολυτεχνείο (ΕΜΠ)","National Technical University of Athens (NTUA)"]},{"key":"dc:type","label":"Dc Type","values":["PhD Thesis"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["Beach rocks","CRETE ISLAND","Faults","PLATFORMS","QUATERNARY","SHORELINES","TECTONIC BLOCKS","TECTONIC DEFORMATION","TERRACES","VERTICAL TECTONIC MOVEMENTS","ΑΚΤΟΓΡΑΜΜΕΣ","ΑΝΑΒΑΘΜΙΔΕΣ","ΕΠΙΦΑΝΕΙΕΣ ΙΣΟΠΕΔΩΣΗΣ","ΚΑΤΑΚΟΡΥΦΕΣ ΤΕΚΤΟΝΙΚΕΣ ΚΙΝΗΣΕΙΣ","Κρήτη","Ρήγματα","ΤΕΚΤΟΝΙΚΑ ΤΕΜΑΧΗ","ΤΕΚΤΟΝΙΚΕΣ ΠΑΡΑΜΟΡΦΩΣΕΙΣ","ΤΕΤΑΡΤΟΓΕΝΕΣ","Engineering and Technology","Environmental Engineering","Επιστήμες Μηχανικού και Τεχνολογία","Περιβαλλοντική Μηχανική"]}]},{"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/1400","http://hdl.handle.net/10442/hedi/1400"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["THE SYSTEMATIC STUDY OF QUATERNARY MARINE PLATFORMS, PLEISTOCENE TERRACES, FAULTS, BEACH-ROCKS, HOLOCENE SHORELINES AND NEARSHORE ARCHAEOLOGICAL REMAINS AND FOUNDINGS ALLOWED US TO DETERMINE THE DIRECTION AND MAGNITUDE OF THE VERTICAL TECTONIC MOVEMENTS AND TECTONIC DEFORMATIONS THAT THE COASTS OF CENTRAL AND EASTERN PART OF CRETE ISLAND HAVE BEEN AFFECTED DURING QUATERNARY AND TO ARRIVE INTOCONCLUSIONS CONTRIBUTING TO THE RECENT GEOLOGICAL EVOLUTION OF THE ISLAND. (SHORTENED)","Η ΣΥΣΤΗΜΑΤΙΚΗ ΜΕΛΕΤΗ ΤΩΝ ΘΑΛΑΣΣΙΩΝ ΤΕΤΑΡΤΟΓΕΝΩΝ ΕΠΙΦΑΝΕΙΩΝ ΙΣΟΠΕΔΩΣΗΣ, ΤΩΝ ΠΛΕΙΣΤΟΚΑΙΝΙΚΩΝ ΑΝΑΒΑΘΜΙΔΩΝ, ΤΩΝ ΡΗΓΜΑΤΩΝ, ΤΩΝ BEACH-ROCKS, ΤΩΝ ΟΛΟΚΑΙΝΙΚΩΝ ΑΚΤΟΓΡΑΜΜΩΝ ΚΑΙ ΤΩΝ ΠΑΡΑΚΤΙΩΝ ΑΡΧΑΙΟΛΟΓΙΚΩΝ ΕΡΕΙΠΙΩΝ ΚΑΙ ΕΥΡΗΜΑΤΩΝ, ΜΑΣ ΕΠΕΤΡΕΨΕ ΝΑ ΚΑΘΟΡΙΣΟΥΜΕ ΤΗ ΦΟΡΑ ΚΑΙ ΤΟ ΜΕΓΕΘΟΣ ΤΩΝ ΚΑΤΑΚΟΡΥΦΩΝ ΤΕΚΤΟΝΙΚΩΝ ΚΙΝΗΣΕΩΝ ΚΑΙ ΤΩΝ ΤΕΚΤΟΝΙΚΩΝ ΠΑΡΑΜΟΡΦΩΣΕΩΝ ΠΟΥ ΕΧΟΥΝ ΥΠΟΣΤΕΙ ΟΙ ΑΚΤΕΣ ΤΟΥ ΚΕΝΤΡΙΚΟΥ ΚΑΙ ΑΝΑΤΟΛΙΚΟΥ ΤΜΗΜΑΤΟΣ ΤΗΣ ΚΡΗΤΗΣ ΣΤΗ ΔΙΑΡΚΕΙΑ ΤΟΥ ΤΕΤΑΡΤΟΓΕΝΟΥΣ ΚΑΙ ΝΑ ΔΙΑΤΥΠΩΣΟΥΜΕ ΣΥΜΠΕΡΑΣΜΑΤΑ ΠΟΥ ΣΥΜΒΑΛΛΟΥΝ ΣΤΗ ΓΝΩΣΗ ΤΗΣ ΠΡΟΣΦΑΤΗΣ ΓΕΩΛΟΓΙΚΗΣ ΕΞΕΛΙΞΗΣ ΤΟΥ ΝΗΣΙΟΥ. (ΠΕΡΙΚΟΠΗ)"]},{"key":"dc:title","label":"Title","values":["ΤΕΚΤΟΝΙΚΕΣ ΚΙΝΗΣΕΙΣ ΚΑΤΑ ΤΟ ΤΕΤΑΡΤΟΓΕΝΕΣ ΣΤΙΣ ΑΚΤΕΣ ΤΗΣ ΑΝΑΤΟΛΙΚΗΣ ΚΡΗΤΗΣ"]}]}],"canonical_facts":{"dc:creator":["Μουρτζάς, Νικόλαος"],"dc:date":["1990"],"dc:description":["THE SYSTEMATIC STUDY OF QUATERNARY MARINE PLATFORMS, PLEISTOCENE TERRACES, FAULTS, BEACH-ROCKS, HOLOCENE SHORELINES AND NEARSHORE ARCHAEOLOGICAL REMAINS AND FOUNDINGS ALLOWED US TO DETERMINE THE DIRECTION AND MAGNITUDE OF THE VERTICAL TECTONIC MOVEMENTS AND TECTONIC DEFORMATIONS THAT THE COASTS OF CENTRAL AND EASTERN PART OF CRETE ISLAND HAVE BEEN AFFECTED DURING QUATERNARY AND TO ARRIVE INTOCONCLUSIONS CONTRIBUTING TO THE RECENT GEOLOGICAL EVOLUTION OF THE ISLAND. (SHORTENED)","Η ΣΥΣΤΗΜΑΤΙΚΗ ΜΕΛΕΤΗ ΤΩΝ ΘΑΛΑΣΣΙΩΝ ΤΕΤΑΡΤΟΓΕΝΩΝ ΕΠΙΦΑΝΕΙΩΝ ΙΣΟΠΕΔΩΣΗΣ, ΤΩΝ ΠΛΕΙΣΤΟΚΑΙΝΙΚΩΝ ΑΝΑΒΑΘΜΙΔΩΝ, ΤΩΝ ΡΗΓΜΑΤΩΝ, ΤΩΝ BEACH-ROCKS, ΤΩΝ ΟΛΟΚΑΙΝΙΚΩΝ ΑΚΤΟΓΡΑΜΜΩΝ ΚΑΙ ΤΩΝ ΠΑΡΑΚΤΙΩΝ ΑΡΧΑΙΟΛΟΓΙΚΩΝ ΕΡΕΙΠΙΩΝ ΚΑΙ ΕΥΡΗΜΑΤΩΝ, ΜΑΣ ΕΠΕΤΡΕΨΕ ΝΑ ΚΑΘΟΡΙΣΟΥΜΕ ΤΗ ΦΟΡΑ ΚΑΙ ΤΟ ΜΕΓΕΘΟΣ ΤΩΝ ΚΑΤΑΚΟΡΥΦΩΝ ΤΕΚΤΟΝΙΚΩΝ ΚΙΝΗΣΕΩΝ ΚΑΙ ΤΩΝ ΤΕΚΤΟΝΙΚΩΝ ΠΑΡΑΜΟΡΦΩΣΕΩΝ ΠΟΥ ΕΧΟΥΝ ΥΠΟΣΤΕΙ ΟΙ ΑΚΤΕΣ ΤΟΥ ΚΕΝΤΡΙΚΟΥ ΚΑΙ ΑΝΑΤΟΛΙΚΟΥ ΤΜΗΜΑΤΟΣ ΤΗΣ ΚΡΗΤΗΣ ΣΤΗ ΔΙΑΡΚΕΙΑ ΤΟΥ ΤΕΤΑΡΤΟΓΕΝΟΥΣ ΚΑΙ ΝΑ ΔΙΑΤΥΠΩΣΟΥΜΕ ΣΥΜΠΕΡΑΣΜΑΤΑ ΠΟΥ ΣΥΜΒΑΛΛΟΥΝ ΣΤΗ ΓΝΩΣΗ ΤΗΣ ΠΡΟΣΦΑΤΗΣ ΓΕΩΛΟΓΙΚΗΣ ΕΞΕΛΙΞΗΣ ΤΟΥ ΝΗΣΙΟΥ. (ΠΕΡΙΚΟΠΗ)"],"dc:identifier":["10.12681/eadd/1400","http://hdl.handle.net/10442/hedi/1400"],"dc:language":["gre"],"dc:publisher":["Εθνικό Μετσόβιο Πολυτεχνείο (ΕΜΠ)","National Technical University of Athens (NTUA)"],"dc:subject":["Beach rocks","CRETE ISLAND","Faults","PLATFORMS","QUATERNARY","SHORELINES","TECTONIC BLOCKS","TECTONIC DEFORMATION","TERRACES","VERTICAL TECTONIC MOVEMENTS","ΑΚΤΟΓΡΑΜΜΕΣ","ΑΝΑΒΑΘΜΙΔΕΣ","ΕΠΙΦΑΝΕΙΕΣ ΙΣΟΠΕΔΩΣΗΣ","ΚΑΤΑΚΟΡΥΦΕΣ ΤΕΚΤΟΝΙΚΕΣ ΚΙΝΗΣΕΙΣ","Κρήτη","Ρήγματα","ΤΕΚΤΟΝΙΚΑ ΤΕΜΑΧΗ","ΤΕΚΤΟΝΙΚΕΣ ΠΑΡΑΜΟΡΦΩΣΕΙΣ","ΤΕΤΑΡΤΟΓΕΝΕΣ","Engineering and Technology","Environmental Engineering","Επιστήμες Μηχανικού και Τεχνολογία","Περιβαλλοντική Μηχανική"],"dc:title":["ΤΕΚΤΟΝΙΚΕΣ ΚΙΝΗΣΕΙΣ ΚΑΤΑ ΤΟ ΤΕΤΑΡΤΟΓΕΝΕΣ ΣΤΙΣ ΑΚΤΕΣ ΤΗΣ ΑΝΑΤΟΛΙΚΗΣ ΚΡΗΤΗΣ"],"dc:type":["PhD Thesis"]},"updated_at":"2026-07-24T02:24:52Z"}