{"id":{"repo_id":"greece","oai_identifier":"oai:10442/1068"},"canonical_url":"https://search.dev.ndltd.org/etd/greece/oai:10442/1068","repository":{"repo_id":"greece","name":"Greek National Archive of PhD Theses","base_url":"https://phdtheses.ekt.gr/eadd_oai/request"},"display":{"title":"ΧΑΡΑΚΤΗΡΙΣΤΙΚΕΣ ΠΑΡΑΜΕΤΡΟΙ ΣΕΙΣΜΙΚΗΣ ΠΗΓΗΣ ΜΕ ΤΗ ΜΕΘΟΔΟ ΤΗΣ ΑΝΤΙΣΤΡΟΦΗΣ ΤΩΝ ΚΥΜΑΤΩΝ ΧΩΡΟΥ: ΕΛΛΑΔΑ ΚΑΙ Η ΕΥΡΥΤΕΡΗ ΠΕΡΙΟΧΗ ΤΗΣ","abstract":"TWENTY FIVE, MODERATE AND LARGE GREEK EARTHQUAKES HAVE BEEN ANALYZED TO YIELD SOURCE PARAMETERS. AN INVERSION TECHNIQUE OF TELESEISMIC BODY WAVES WAS USED FORRECORDINGS AT 30-90. RECORDING FROM 12-16 STATIONS OF P AND SH WAVEFORMS HAVE BEEN INVERTED SIMULTANEOUSLY, TO GIVE FOCAL MECHANISMS, SOURCE DURATION, RAPTURE COMPLEXITY, SEISMIC MOMENT AND STRESS DROP. FIVE AREAS HAVE BEEN RECOGNIZED IN THE GREEK REGION WITH SEPARATE SOURCE PROPERTIES. EARTHQUAKES CAUSED BY NORMAL FAULTING HAVE RELATIVELY SIMPLE RAPTURE PROCESS COMPARED TO THE ONES DUE TO TRANSFORM FAULTS AND DURATION OF THE SOURCE CLOSE TO 10 SEC. EARTHQUAKES AT DEPTHS MORE THAN 25 KM ARE IMPULSIVE IN THEIR RAPTURE PROCESS. THE COMPUTED AVERAGESTRESS DROP IS AT LEAST ONE ORDER OF MAGNITUDE LESS THAN THE STRESS DROP CALCULATED FOR THE INDIVIDUAL ASPERITIES RECOGNIZED IN THE RAPTURE PROCESS. SOURCE PARAMETERS HAVE BEEN CALCULATED WITH THE MOST RELIABLE COMPUTATIONAL TECHNIQUE TO DATE.","abstract_html":"TWENTY FIVE, MODERATE AND LARGE GREEK EARTHQUAKES HAVE BEEN ANALYZED TO YIELD SOURCE PARAMETERS. AN INVERSION TECHNIQUE OF TELESEISMIC BODY WAVES WAS USED FORRECORDINGS AT 30-90. RECORDING FROM 12-16 STATIONS OF P AND SH WAVEFORMS HAVE BEEN INVERTED SIMULTANEOUSLY, TO GIVE FOCAL MECHANISMS, SOURCE DURATION, RAPTURE COMPLEXITY, SEISMIC MOMENT AND STRESS DROP. FIVE AREAS HAVE BEEN RECOGNIZED IN THE GREEK REGION WITH SEPARATE SOURCE PROPERTIES. EARTHQUAKES CAUSED BY NORMAL FAULTING HAVE RELATIVELY SIMPLE RAPTURE PROCESS COMPARED TO THE ONES DUE TO TRANSFORM FAULTS AND DURATION OF THE SOURCE CLOSE TO 10 SEC. EARTHQUAKES AT DEPTHS MORE THAN 25 KM ARE IMPULSIVE IN THEIR RAPTURE PROCESS. THE COMPUTED AVERAGESTRESS DROP IS AT LEAST ONE ORDER OF MAGNITUDE LESS THAN THE STRESS DROP CALCULATED FOR THE INDIVIDUAL ASPERITIES RECOGNIZED IN THE RAPTURE PROCESS. SOURCE PARAMETERS HAVE BEEN CALCULATED WITH THE MOST RELIABLE COMPUTATIONAL TECHNIQUE TO DATE.","abstract_has_math":false,"creators":["Ιωαννίδου, Ελένη"],"institution":"Εθνικό και Καποδιστριακό Πανεπιστήμιο Αθηνών (ΕΚΠΑ)","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":"2026-07-24T02:24:43Z","subjects":["COMPLEXITY OF THE SEISMIC SOURCE","Focal mechanisms","GREEK EARTHQUAKES","Inversion","LEAST SQUARE INVERSTON","SOURCE DURATION","Source parameters","STRESS DROP","TELESEISMIC BODY WAVES ANALYSIS","Ελλάδα","ΚΟΡΙΝΘΙΑΚΟΣ, ΙΟΝΙΟ, ΚΕΦΑΛΛΟΝΙΑ, ΚΡΗΤΗ, ΑΙΓΑΙΟ","ΜΕΘΟΔΟΣ ΕΛΑΧΙΣΤΩΝ ΤΕΤΡΑΓΩΝΩΝ","ΜΕΘΟΔΟΣΑΝΤΙΣΤΡΟΦΗΣ","Μηχανισμοί γένεσης","ΠΑΡΑΜΕΤΡΟΙ ΣΕΙΣΜΙΚΗΣ ΠΗΓΗΣ","ΠΤΩΣΗ ΤΑΣΗΣ ΣΤΗ ΠΗΓΗ","ΣΕΙΣΜΙΚΗ ΠΗΓΗ","ΣΕΙΣΜΟΙ ΕΛΛΗΝΙΚΟΥ ΧΩΡΟΥ","ΤΑΥΤΙΣΗ ΚΥΜΑΤΟΜΟΡΦΩΝ","ΧΡΟΝΙΚΗ ΕΞΕΛΙΞΗ ΠΗΓΗΣ","Φυσικές Επιστήμες","Natural Sciences","Γεωεπιστήμες και Επιστήμες Περιβάλλοντος","Earth and Related Environmental Sciences"],"languages":["gre"],"rights":[],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier","label":"Identifier","values":["10.12681/eadd/1068"],"render_values":[{"text":"10.12681/eadd/1068","href":"https://doi.org/10.12681/eadd/1068","code":true}]}]},"links":{"outbound_url":"http://hdl.handle.net/10442/hedi/1068","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:creator","label":"Author","values":["Ιωαννίδου, Ελένη"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["1989"]},{"key":"dc:publisher","label":"Institution","values":["Εθνικό και Καποδιστριακό Πανεπιστήμιο Αθηνών (ΕΚΠΑ)","National and Kapodistrian University of Athens"]},{"key":"dc:type","label":"Dc Type","values":["PhD Thesis"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["COMPLEXITY OF THE SEISMIC SOURCE","Focal mechanisms","GREEK EARTHQUAKES","Inversion","LEAST SQUARE INVERSTON","SOURCE DURATION","Source parameters","STRESS DROP","TELESEISMIC BODY WAVES ANALYSIS","Ελλάδα","ΚΟΡΙΝΘΙΑΚΟΣ, ΙΟΝΙΟ, ΚΕΦΑΛΛΟΝΙΑ, ΚΡΗΤΗ, ΑΙΓΑΙΟ","ΜΕΘΟΔΟΣ ΕΛΑΧΙΣΤΩΝ ΤΕΤΡΑΓΩΝΩΝ","ΜΕΘΟΔΟΣΑΝΤΙΣΤΡΟΦΗΣ","Μηχανισμοί γένεσης","ΠΑΡΑΜΕΤΡΟΙ ΣΕΙΣΜΙΚΗΣ ΠΗΓΗΣ","ΠΤΩΣΗ ΤΑΣΗΣ ΣΤΗ ΠΗΓΗ","ΣΕΙΣΜΙΚΗ ΠΗΓΗ","ΣΕΙΣΜΟΙ ΕΛΛΗΝΙΚΟΥ ΧΩΡΟΥ","ΤΑΥΤΙΣΗ ΚΥΜΑΤΟΜΟΡΦΩΝ","ΧΡΟΝΙΚΗ ΕΞΕΛΙΞΗ ΠΗΓΗΣ","Φυσικές Επιστήμες","Natural Sciences","Γεωεπιστήμες και Επιστήμες Περιβάλλοντος","Earth and Related Environmental Sciences"]}]},{"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/1068","http://hdl.handle.net/10442/hedi/1068"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["TWENTY FIVE, MODERATE AND LARGE GREEK EARTHQUAKES HAVE BEEN ANALYZED TO YIELD SOURCE PARAMETERS. AN INVERSION TECHNIQUE OF TELESEISMIC BODY WAVES WAS USED FORRECORDINGS AT 30-90. RECORDING FROM 12-16 STATIONS OF P AND SH WAVEFORMS HAVE BEEN INVERTED SIMULTANEOUSLY, TO GIVE FOCAL MECHANISMS, SOURCE DURATION, RAPTURE COMPLEXITY, SEISMIC MOMENT AND STRESS DROP. FIVE AREAS HAVE BEEN RECOGNIZED IN THE GREEK REGION WITH SEPARATE SOURCE PROPERTIES. EARTHQUAKES CAUSED BY NORMAL FAULTING HAVE RELATIVELY SIMPLE RAPTURE PROCESS COMPARED TO THE ONES DUE TO TRANSFORM FAULTS AND DURATION OF THE SOURCE CLOSE TO 10 SEC. EARTHQUAKES AT DEPTHS MORE THAN 25 KM ARE IMPULSIVE IN THEIR RAPTURE PROCESS. THE COMPUTED AVERAGESTRESS DROP IS AT LEAST ONE ORDER OF MAGNITUDE LESS THAN THE STRESS DROP CALCULATED FOR THE INDIVIDUAL ASPERITIES RECOGNIZED IN THE RAPTURE PROCESS. SOURCE PARAMETERS HAVE BEEN CALCULATED WITH THE MOST RELIABLE COMPUTATIONAL TECHNIQUE TO DATE.","ΕΙΚΟΣΙ ΠΕΝΤΕ ΜΕΓΑΛΟΙ ΣΕΙΣΜΟΙ (MS>5.8) ΤΟΥ ΕΛΛΗΝΙΚΟΥ ΧΩΡΟΥ ΑΝΑΛΥΘΗΚΑΝ ΜΕ ΤΗΝ ΤΕΧΝΙΚΗ ΤΗΣ ΑΝΤΙΣΤΡΟΦΗΣ ΤΩΝ ΚΥΜΑΤΩΝ ΧΩΡΟΥ ΑΠΟ ΤΗΛΕΜΕΤΡΙΚΕΣ ΑΠΟΣΤΑΣΕΙΣ (30-90). ΚΑΤΑ ΜΕΣΟ ΟΡΟ 12-16 ΣΤΑΘΜΟΙ (ΚΑΤΑΓΡΑΦΕΣ P-SH ΚΥΜΑΤΩΝ) ΧΡΗΣΙΜΟΠΟΙΗΘΗΚΑΝ ΓΙΑ ΤΗΝ ΕΠΕΞΕΡΓΑΣΙΑ ΚΑΘΕΝΟΣ ΑΠΟ ΤΟΥΣ ΣΕΙΣΜΟΥΣ ΚΑΙ ΠΡΟΕΚΥΨΑΝ ΟΙ ΠΑΡΑΜΕΤΡΟΙ ΠΗΓΗΣ. ΥΠΟΛΟΓΙΣΤΗΚΑΝ, ΟΙ ΜΗΧΑΝΙΣΜΟΙ ΓΕΝΕΣΗΣ, ΟΙ ΣΕΙΣΜΙΚΕΣ ΡΟΠΕΣ, Η ΔΙΑΡΚΕΙΑ ΤΩΝ ΠΗΓΩΝ, Η ΠΟΛΥΠΛΟΚΟΤΗΤΑ ΤΗΣ ΔΙΑΡΡΗΞΗΣ ΣΤΗΝ ΠΗΓΗ, ΜΕ ΜΕΓΑΛΗ ΑΚΡΙΒΕΙΑ. ΑΠΟ ΤΙΣ ΠΕΡΙΟΧΕΣ ΣΤΙΣ ΟΠΟΙΕΣ ΟΜΑΔΟΠΟΙΟΥΝΤΑΙ ΟΙ ΣΕΙΣΜΟΙ ΕΙΝΑΙ ΦΑΝΕΡΟ ΟΤΙ ΣΕΙΣΜΟΙ ΑΠΟ ΚΑΝΟΝΙΚΑ ΡΗΓΜΑΤΑ ΠΑΡΟΥΣΙΑΖΟΥΝ ΣΧΕΤΙΚΑ ΑΠΛΗ ΔΙΑΡΡΗΞΗ ΜΕ ΧΡΟΝΙΚΗ ΔΙΑΡΚΕΙΑ ΠΕΡΙΠΟΥ 10 SEC. ΑΝΤΙΘΕΤΑ, ΣΕΙΣΜΟΙ ΑΠΟ ΡΗΓΜΑΤΑ ΜΕΤΑΣΧΗΜΑΤΙΣΜΟΥ ΕΙΝΑΙ ΙΔΙΑΙΤΕΡΑ ΠΟΛΥΠΛΟΚΑ ΣΤΗ ΔΙΑΔΙΚΑΣΙΑ ΤΗΣ ΔΙΑΡΡΗΞΗΣ, ΕΝΩ ΟΙ ΣΕΙΣΜΟΙ ΜΕ ΒΑΘΟΣ ΜΕΓΑΛΥΤΕΡΟ ΤΩΝ 25 ΚΜ ΕΧΟΥΝ ΩΣΤΙΚΟ ΧΑΡΑΚΤΗΡΑ ΔΙΑΡΡΗΞΗΣ. Η ΜΕΣΗ ΠΤΩΣΗ ΤΑΣΗΣ ΕΙΝΑΙ ΓΙΑ ΤΟ ΣΥΝΟΛΟ ΤΩΝ ΣΕΙΣΜΩΝ ΤΟΥΛΑΧΙΣΤΟΝ ΜΙΑΣ ΤΑΞΗΣ ΜΕΓΕΘΟΥΣ ΜΙΚΡΟΤΕΡΗ ΑΠΟ ΑΥΤΗ ΠΟΥ ΥΠΟΛΟΓΙΖΕΤΑΙ ΓΙΑ ΤΗΝ ΠΤΩΣΗ ΤΑΣΗΣ ΣΤΑ ΙΔΙΑΙΤΕΡΑ ΤΜΗΜΑΤΑ ΥΨΗΛΩΝ ΤΑΣΕΩΝ ΠΟΥ ΠΑΡΟΥΣΙΑΖΟΝΤΑΙ ΣΤΗ ΔΙΑΔΙΚΑΣΙΑ ΤΗΣ ΡΗΓΜΑΤΩΣΗΣ."]},{"key":"dc:title","label":"Title","values":["ΧΑΡΑΚΤΗΡΙΣΤΙΚΕΣ ΠΑΡΑΜΕΤΡΟΙ ΣΕΙΣΜΙΚΗΣ ΠΗΓΗΣ ΜΕ ΤΗ ΜΕΘΟΔΟ ΤΗΣ ΑΝΤΙΣΤΡΟΦΗΣ ΤΩΝ ΚΥΜΑΤΩΝ ΧΩΡΟΥ: ΕΛΛΑΔΑ ΚΑΙ Η ΕΥΡΥΤΕΡΗ ΠΕΡΙΟΧΗ ΤΗΣ","SEISMIC SOURCE PARAMETERS FROM INVERSION OF TELESEISMIC BODYWAVES: ALL MODERATEAND LARGE GREEK EARTHQUAKES FOR THE YEARS 1965-1988"]}]}],"canonical_facts":{"dc:creator":["Ιωαννίδου, Ελένη"],"dc:date":["1989"],"dc:description":["TWENTY FIVE, MODERATE AND LARGE GREEK EARTHQUAKES HAVE BEEN ANALYZED TO YIELD SOURCE PARAMETERS. AN INVERSION TECHNIQUE OF TELESEISMIC BODY WAVES WAS USED FORRECORDINGS AT 30-90. RECORDING FROM 12-16 STATIONS OF P AND SH WAVEFORMS HAVE BEEN INVERTED SIMULTANEOUSLY, TO GIVE FOCAL MECHANISMS, SOURCE DURATION, RAPTURE COMPLEXITY, SEISMIC MOMENT AND STRESS DROP. FIVE AREAS HAVE BEEN RECOGNIZED IN THE GREEK REGION WITH SEPARATE SOURCE PROPERTIES. EARTHQUAKES CAUSED BY NORMAL FAULTING HAVE RELATIVELY SIMPLE RAPTURE PROCESS COMPARED TO THE ONES DUE TO TRANSFORM FAULTS AND DURATION OF THE SOURCE CLOSE TO 10 SEC. EARTHQUAKES AT DEPTHS MORE THAN 25 KM ARE IMPULSIVE IN THEIR RAPTURE PROCESS. THE COMPUTED AVERAGESTRESS DROP IS AT LEAST ONE ORDER OF MAGNITUDE LESS THAN THE STRESS DROP CALCULATED FOR THE INDIVIDUAL ASPERITIES RECOGNIZED IN THE RAPTURE PROCESS. SOURCE PARAMETERS HAVE BEEN CALCULATED WITH THE MOST RELIABLE COMPUTATIONAL TECHNIQUE TO DATE.","ΕΙΚΟΣΙ ΠΕΝΤΕ ΜΕΓΑΛΟΙ ΣΕΙΣΜΟΙ (MS>5.8) ΤΟΥ ΕΛΛΗΝΙΚΟΥ ΧΩΡΟΥ ΑΝΑΛΥΘΗΚΑΝ ΜΕ ΤΗΝ ΤΕΧΝΙΚΗ ΤΗΣ ΑΝΤΙΣΤΡΟΦΗΣ ΤΩΝ ΚΥΜΑΤΩΝ ΧΩΡΟΥ ΑΠΟ ΤΗΛΕΜΕΤΡΙΚΕΣ ΑΠΟΣΤΑΣΕΙΣ (30-90). ΚΑΤΑ ΜΕΣΟ ΟΡΟ 12-16 ΣΤΑΘΜΟΙ (ΚΑΤΑΓΡΑΦΕΣ P-SH ΚΥΜΑΤΩΝ) ΧΡΗΣΙΜΟΠΟΙΗΘΗΚΑΝ ΓΙΑ ΤΗΝ ΕΠΕΞΕΡΓΑΣΙΑ ΚΑΘΕΝΟΣ ΑΠΟ ΤΟΥΣ ΣΕΙΣΜΟΥΣ ΚΑΙ ΠΡΟΕΚΥΨΑΝ ΟΙ ΠΑΡΑΜΕΤΡΟΙ ΠΗΓΗΣ. ΥΠΟΛΟΓΙΣΤΗΚΑΝ, ΟΙ ΜΗΧΑΝΙΣΜΟΙ ΓΕΝΕΣΗΣ, ΟΙ ΣΕΙΣΜΙΚΕΣ ΡΟΠΕΣ, Η ΔΙΑΡΚΕΙΑ ΤΩΝ ΠΗΓΩΝ, Η ΠΟΛΥΠΛΟΚΟΤΗΤΑ ΤΗΣ ΔΙΑΡΡΗΞΗΣ ΣΤΗΝ ΠΗΓΗ, ΜΕ ΜΕΓΑΛΗ ΑΚΡΙΒΕΙΑ. ΑΠΟ ΤΙΣ ΠΕΡΙΟΧΕΣ ΣΤΙΣ ΟΠΟΙΕΣ ΟΜΑΔΟΠΟΙΟΥΝΤΑΙ ΟΙ ΣΕΙΣΜΟΙ ΕΙΝΑΙ ΦΑΝΕΡΟ ΟΤΙ ΣΕΙΣΜΟΙ ΑΠΟ ΚΑΝΟΝΙΚΑ ΡΗΓΜΑΤΑ ΠΑΡΟΥΣΙΑΖΟΥΝ ΣΧΕΤΙΚΑ ΑΠΛΗ ΔΙΑΡΡΗΞΗ ΜΕ ΧΡΟΝΙΚΗ ΔΙΑΡΚΕΙΑ ΠΕΡΙΠΟΥ 10 SEC. ΑΝΤΙΘΕΤΑ, ΣΕΙΣΜΟΙ ΑΠΟ ΡΗΓΜΑΤΑ ΜΕΤΑΣΧΗΜΑΤΙΣΜΟΥ ΕΙΝΑΙ ΙΔΙΑΙΤΕΡΑ ΠΟΛΥΠΛΟΚΑ ΣΤΗ ΔΙΑΔΙΚΑΣΙΑ ΤΗΣ ΔΙΑΡΡΗΞΗΣ, ΕΝΩ ΟΙ ΣΕΙΣΜΟΙ ΜΕ ΒΑΘΟΣ ΜΕΓΑΛΥΤΕΡΟ ΤΩΝ 25 ΚΜ ΕΧΟΥΝ ΩΣΤΙΚΟ ΧΑΡΑΚΤΗΡΑ ΔΙΑΡΡΗΞΗΣ. Η ΜΕΣΗ ΠΤΩΣΗ ΤΑΣΗΣ ΕΙΝΑΙ ΓΙΑ ΤΟ ΣΥΝΟΛΟ ΤΩΝ ΣΕΙΣΜΩΝ ΤΟΥΛΑΧΙΣΤΟΝ ΜΙΑΣ ΤΑΞΗΣ ΜΕΓΕΘΟΥΣ ΜΙΚΡΟΤΕΡΗ ΑΠΟ ΑΥΤΗ ΠΟΥ ΥΠΟΛΟΓΙΖΕΤΑΙ ΓΙΑ ΤΗΝ ΠΤΩΣΗ ΤΑΣΗΣ ΣΤΑ ΙΔΙΑΙΤΕΡΑ ΤΜΗΜΑΤΑ ΥΨΗΛΩΝ ΤΑΣΕΩΝ ΠΟΥ ΠΑΡΟΥΣΙΑΖΟΝΤΑΙ ΣΤΗ ΔΙΑΔΙΚΑΣΙΑ ΤΗΣ ΡΗΓΜΑΤΩΣΗΣ."],"dc:identifier":["10.12681/eadd/1068","http://hdl.handle.net/10442/hedi/1068"],"dc:language":["gre"],"dc:publisher":["Εθνικό και Καποδιστριακό Πανεπιστήμιο Αθηνών (ΕΚΠΑ)","National and Kapodistrian University of Athens"],"dc:subject":["COMPLEXITY OF THE SEISMIC SOURCE","Focal mechanisms","GREEK EARTHQUAKES","Inversion","LEAST SQUARE INVERSTON","SOURCE DURATION","Source parameters","STRESS DROP","TELESEISMIC BODY WAVES ANALYSIS","Ελλάδα","ΚΟΡΙΝΘΙΑΚΟΣ, ΙΟΝΙΟ, ΚΕΦΑΛΛΟΝΙΑ, ΚΡΗΤΗ, ΑΙΓΑΙΟ","ΜΕΘΟΔΟΣ ΕΛΑΧΙΣΤΩΝ ΤΕΤΡΑΓΩΝΩΝ","ΜΕΘΟΔΟΣΑΝΤΙΣΤΡΟΦΗΣ","Μηχανισμοί γένεσης","ΠΑΡΑΜΕΤΡΟΙ ΣΕΙΣΜΙΚΗΣ ΠΗΓΗΣ","ΠΤΩΣΗ ΤΑΣΗΣ ΣΤΗ ΠΗΓΗ","ΣΕΙΣΜΙΚΗ ΠΗΓΗ","ΣΕΙΣΜΟΙ ΕΛΛΗΝΙΚΟΥ ΧΩΡΟΥ","ΤΑΥΤΙΣΗ ΚΥΜΑΤΟΜΟΡΦΩΝ","ΧΡΟΝΙΚΗ ΕΞΕΛΙΞΗ ΠΗΓΗΣ","Φυσικές Επιστήμες","Natural Sciences","Γεωεπιστήμες και Επιστήμες Περιβάλλοντος","Earth and Related Environmental Sciences"],"dc:title":["ΧΑΡΑΚΤΗΡΙΣΤΙΚΕΣ ΠΑΡΑΜΕΤΡΟΙ ΣΕΙΣΜΙΚΗΣ ΠΗΓΗΣ ΜΕ ΤΗ ΜΕΘΟΔΟ ΤΗΣ ΑΝΤΙΣΤΡΟΦΗΣ ΤΩΝ ΚΥΜΑΤΩΝ ΧΩΡΟΥ: ΕΛΛΑΔΑ ΚΑΙ Η ΕΥΡΥΤΕΡΗ ΠΕΡΙΟΧΗ ΤΗΣ","SEISMIC SOURCE PARAMETERS FROM INVERSION OF TELESEISMIC BODYWAVES: ALL MODERATEAND LARGE GREEK EARTHQUAKES FOR THE YEARS 1965-1988"],"dc:type":["PhD Thesis"]},"updated_at":"2026-07-24T02:24:43Z"}