{"id":{"repo_id":"greece","oai_identifier":"oai:10442/1268"},"canonical_url":"https://search.dev.ndltd.org/etd/greece/oai:10442/1268","repository":{"repo_id":"greece","name":"Greek National Archive of PhD Theses","base_url":"https://phdtheses.ekt.gr/eadd_oai/request"},"display":{"title":"ΘΕΡΜΟΜΗΧΑΝΙΚΗ ΣΥΜΠΕΡΙΦΟΡΑ ΤΗΣ ΛΙΘΟΣΦΑΙΡΑΣ ΣΤΟΝ ΕΛΛΗΝΙΚΟ ΧΩΡΟ","abstract":"A QUANTITATIVE STUDY OF BOTH THE THERMAL AND MECHANICAL STATE OF THE LITHOSPHERE IN GREECE AND THEIR INTERRELATIONSHIP IN THE COURSE OF THE GEOLOGIC TIME. THEMAIN DATA USED ARE NEOTECTONIC ONES, ABSOLUTE VALUES OF THE EFFECTIVE PRINCIPAL STRESSES MEASURED THROUGH HYDROFRACTURING IN OIL WELLS, THE TECTONIC SUBSIDENCE OF NEOGENE SEDIMENTARY BASINS, TEMPERATURE MEASUREMENTS AND ESTIMATED HEAT FLOW, PALEOGEOTHERMAL INDICATORS, DEEP GEOPHYSICAL DATA RELATED TO THE CRUST STRUCTURE, RHEOLOGICAL MODELS FOR THE STRENGTH OF THE LITHOSPHERE. OFFSHORE AND WEST OF PARGA THE VERTICAL PRINCIPAL STRESS (ΣΝ) IS INTERMEDIATE BETWEEN ΣΗ AND ΣΗ, IN NW PELOPONNESE ΣΝ EXCEEDS ΣΗ WITH A SLIGHT DIFFERENCY ONLY, WHEREAS IT ISΣΝ>>ΣΗ>ΣΗ IN THE NORTH AEGEAN. A COMPRESSIVE TECTONIC STRESS OF ABOUT 10 MPA IS ESTIMATED FOR WESTERN GREECE, IN CONTRAST WITH AN EXTENSIVE STRESS OF ABOUT 3MPA IN THE NORTH AEGEAN. TECTONICS PROVINCES WERE DELINIATED IN CLOSE CORRESPONDENCE TO GEOTHERMAL PROVINCES. THE THERMAL STATE AND THE MECHANICAL STRENGTH OF THE AEGEAN LITHOSPHERE WAS STUDIED, AS WELL AS THE THERMAL HISTORY OF WESTERNGREECE. A THINNING FACTOR OF 1,4-1,5 IS ESTIMATED FOR THE NORTH AEGEAN CRUST AND 2,4-9,8 FOR THE MANTTLE. A MODEL OF SUBDUCTION OF THE AFRICAN LITHOSPHERE ISEXAMINED IN RELATIONSHIP TO THE ACTIVE STRESS FIELD, THE THERMAL STATE, THE MIGRATION OF VOLCANISM FROM THRACE TO THE PRESENT POSITION IN THE AEGEAN AND THE FORMATION OF NEOGENE BASINS AND TROUGHS.","abstract_html":"A QUANTITATIVE STUDY OF BOTH THE THERMAL AND MECHANICAL STATE OF THE LITHOSPHERE IN GREECE AND THEIR INTERRELATIONSHIP IN THE COURSE OF THE GEOLOGIC TIME. THEMAIN DATA USED ARE NEOTECTONIC ONES, ABSOLUTE VALUES OF THE EFFECTIVE PRINCIPAL STRESSES MEASURED THROUGH HYDROFRACTURING IN OIL WELLS, THE TECTONIC SUBSIDENCE OF NEOGENE SEDIMENTARY BASINS, TEMPERATURE MEASUREMENTS AND ESTIMATED HEAT FLOW, PALEOGEOTHERMAL INDICATORS, DEEP GEOPHYSICAL DATA RELATED TO THE CRUST STRUCTURE, RHEOLOGICAL MODELS FOR THE STRENGTH OF THE LITHOSPHERE. OFFSHORE AND WEST OF PARGA THE VERTICAL PRINCIPAL STRESS (ΣΝ) IS INTERMEDIATE BETWEEN ΣΗ AND ΣΗ, IN NW PELOPONNESE ΣΝ EXCEEDS ΣΗ WITH A SLIGHT DIFFERENCY ONLY, WHEREAS IT ISΣΝ>>ΣΗ>ΣΗ IN THE NORTH AEGEAN. A COMPRESSIVE TECTONIC STRESS OF ABOUT 10 MPA IS ESTIMATED FOR WESTERN GREECE, IN CONTRAST WITH AN EXTENSIVE STRESS OF ABOUT 3MPA IN THE NORTH AEGEAN. TECTONICS PROVINCES WERE DELINIATED IN CLOSE CORRESPONDENCE TO GEOTHERMAL PROVINCES. THE THERMAL STATE AND THE MECHANICAL STRENGTH OF THE AEGEAN LITHOSPHERE WAS STUDIED, AS WELL AS THE THERMAL HISTORY OF WESTERNGREECE. A THINNING FACTOR OF 1,4-1,5 IS ESTIMATED FOR THE NORTH AEGEAN CRUST AND 2,4-9,8 FOR THE MANTTLE. A MODEL OF SUBDUCTION OF THE AFRICAN LITHOSPHERE ISEXAMINED IN RELATIONSHIP TO THE ACTIVE STRESS FIELD, THE THERMAL STATE, THE MIGRATION OF VOLCANISM FROM THRACE TO THE PRESENT POSITION IN THE AEGEAN AND THE FORMATION OF NEOGENE BASINS AND TROUGHS.","abstract_has_math":false,"creators":["Χιώτης, Ευστάθιος"],"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":"2026-07-24T02:24:49Z","subjects":["Aegean sea","GEOTHERM","HYDROFRACTURING","Oil generation","Pore pressure","REACTIVATION OF FAULTS","SEBDUCTION MODEL IN AEGEAN","STRENGTH OF THE LITHOSPHERE","Stress field","Αιγαίο","ΑΝΑΔΡΑΣΗ ΡΗΓΜΑΤΩΝ","ΑΝΤΟΧΗ ΛΙΘΟΣΦΑΙΡΑΣ","ΑΝΤΟΧΗ ΡΗΓΜΑΤΩΝ","ΓΕΩΘΕΡΜΟΣ","ΕΝΤΑΤΙΚΟ ΠΕΔΙΟ","Πετρελαιογένεση","Πίεση πόρων","ΠΡΟΤΥΠΟ ΥΠΟΒΥΘΙΣΗΣ ΣΤΟ ΑΙΓΑΙΟ","ΣΧΗΜΑΤΙΣΜΟΣ ΙΖΗΜΑΤΟΓΕΝΩΝ ΤΑΦΡΩΝ","ΥΔΡΟΡΩΓΜΑΤΩΣΗ","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/1268"],"render_values":[{"text":"10.12681/eadd/1268","href":"https://doi.org/10.12681/eadd/1268","code":true}]}]},"links":{"outbound_url":"http://hdl.handle.net/10442/hedi/1268","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:creator","label":"Author","values":["Χιώτης, Ευστάθιος"]}]},{"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":["Aegean sea","GEOTHERM","HYDROFRACTURING","Oil generation","Pore pressure","REACTIVATION OF FAULTS","SEBDUCTION MODEL IN AEGEAN","STRENGTH OF THE LITHOSPHERE","Stress field","Αιγαίο","ΑΝΑΔΡΑΣΗ ΡΗΓΜΑΤΩΝ","ΑΝΤΟΧΗ ΛΙΘΟΣΦΑΙΡΑΣ","ΑΝΤΟΧΗ ΡΗΓΜΑΤΩΝ","ΓΕΩΘΕΡΜΟΣ","ΕΝΤΑΤΙΚΟ ΠΕΔΙΟ","Πετρελαιογένεση","Πίεση πόρων","ΠΡΟΤΥΠΟ ΥΠΟΒΥΘΙΣΗΣ ΣΤΟ ΑΙΓΑΙΟ","ΣΧΗΜΑΤΙΣΜΟΣ ΙΖΗΜΑΤΟΓΕΝΩΝ ΤΑΦΡΩΝ","ΥΔΡΟΡΩΓΜΑΤΩΣΗ","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/1268","http://hdl.handle.net/10442/hedi/1268"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["A QUANTITATIVE STUDY OF BOTH THE THERMAL AND MECHANICAL STATE OF THE LITHOSPHERE IN GREECE AND THEIR INTERRELATIONSHIP IN THE COURSE OF THE GEOLOGIC TIME. THEMAIN DATA USED ARE NEOTECTONIC ONES, ABSOLUTE VALUES OF THE EFFECTIVE PRINCIPAL STRESSES MEASURED THROUGH HYDROFRACTURING IN OIL WELLS, THE TECTONIC SUBSIDENCE OF NEOGENE SEDIMENTARY BASINS, TEMPERATURE MEASUREMENTS AND ESTIMATED HEAT FLOW, PALEOGEOTHERMAL INDICATORS, DEEP GEOPHYSICAL DATA RELATED TO THE CRUST STRUCTURE, RHEOLOGICAL MODELS FOR THE STRENGTH OF THE LITHOSPHERE. OFFSHORE AND WEST OF PARGA THE VERTICAL PRINCIPAL STRESS (ΣΝ) IS INTERMEDIATE BETWEEN ΣΗ AND ΣΗ, IN NW PELOPONNESE ΣΝ EXCEEDS ΣΗ WITH A SLIGHT DIFFERENCY ONLY, WHEREAS IT ISΣΝ>>ΣΗ>ΣΗ IN THE NORTH AEGEAN. A COMPRESSIVE TECTONIC STRESS OF ABOUT 10 MPA IS ESTIMATED FOR WESTERN GREECE, IN CONTRAST WITH AN EXTENSIVE STRESS OF ABOUT 3MPA IN THE NORTH AEGEAN. TECTONICS PROVINCES WERE DELINIATED IN CLOSE CORRESPONDENCE TO GEOTHERMAL PROVINCES. THE THERMAL STATE AND THE MECHANICAL STRENGTH OF THE AEGEAN LITHOSPHERE WAS STUDIED, AS WELL AS THE THERMAL HISTORY OF WESTERNGREECE. A THINNING FACTOR OF 1,4-1,5 IS ESTIMATED FOR THE NORTH AEGEAN CRUST AND 2,4-9,8 FOR THE MANTTLE. A MODEL OF SUBDUCTION OF THE AFRICAN LITHOSPHERE ISEXAMINED IN RELATIONSHIP TO THE ACTIVE STRESS FIELD, THE THERMAL STATE, THE MIGRATION OF VOLCANISM FROM THRACE TO THE PRESENT POSITION IN THE AEGEAN AND THE FORMATION OF NEOGENE BASINS AND TROUGHS.","ΠΟΣΟΤΙΚΗ ΜΕΛΕΤΗ ΤΗΣ ΘΕΡΜΙΚΗΣ ΚΑΙ ΤΗΣ ΜΗΧΑΝΙΚΗΣ ΚΑΤΑΣΤΑΣΗΣ ΤΗΣ ΛΙΘΟΣΦΑΙΡΑΣ ΣΤΟΝ ΕΛΛΗΝΙΚΟ ΧΩΡΟ ΚΑΙ ΤΗΣ ΜΕΤΑΞΥ ΤΟΥΣ ΣΧΕΣΕΩΣ ΣΤΗ ΔΙΑΡΚΕΙΑ ΤΟΥ ΓΕΩΛΟΓΙΚΟΥ ΧΡΟΝΟΥ. ΤΑ ΚΥΡΙΑ ΣΤΟΙΧΕΙΑ ΠΟΥ ΧΡΗΣΙΜΟΠΟΙΟΥΝΤΑΙ ΕΙΝΑΙ ΝΕΟΤΕΚΤΟΝΙΚΑ, ΑΠΟΛΥΤΕΣ ΤΙΜΕΣ ΤΩΝ ΕΝΕΡΓΩΝ ΚΥΡΙΩΝ ΤΑΣΕΩΝ ΥΠΟΛΟΓΙΣΜΕΝΕΣ ΑΠΟ ΔΕΔΟΜΕΝΑ ΥΔΡΟΡΩΓΜΑΤΩΣΗΣ ΣΕ ΓΕΩΤΡΗΣΕΙΣ ΠΕΤΡΕΛΑΙΟΥ, Η ΤΕΚΤΟΝΙΚΗ ΣΥΝΙΖΗΣΗ ΝΕΟΓΕΝΩΝ ΙΖΗΜΑΤΟΓΕΝΩΝ ΛΕΚΑΝΩΝ, ΜΕΤΡΗΣΕΙΣ ΘΕΡΜΟΚΡΑΣΙΑΣ ΚΑΙ ΕΚΤΙΜΗΣΕΙΣ ΤΗΣ ΡΟΗΣ ΘΕΡΜΟΤΗΤΟΣ, ΠΑΛΑΙΟΘΕΡΜΙΚΟΙ ΔΕΙΚΤΕΣ, ΓΕΩΦΥΣΙΚΑ ΔΕΔΟΜΕΝΑ ΓΙΑ ΤΗ ΔΟΜΗ ΤΟΥ ΦΛΟΙΟΥ, ΠΡΟΤΥΠΑ ΥΠΟΛΟΓΙΣΜΟΥ ΤΗΣ ΑΝΤΟΧΗΣ ΤΗΣ ΛΙΘΟΣΦΑΙΡΑΣ. ΣΤΗ ΘΑΛΑΣΣΙΑ ΠΕΡΙΟΧΗ ΔΥΤΙΚΑ ΤΗΣ ΠΑΡΓΑΣ Η ΚΑΤΑΚΟΡΥΦΗ ΚΥΡΙΑ ΤΑΣΗ (ΣΝ) ΕΙΝΑΙ ΕΝΔΙΑΜΕΣΗ ΜΕΤΑΞΥ ΣΗ ΚΑΙ ΣΗ, ΣΤΗ ΒΔ ΠΕΛΟΠΟΝΝΗΣΟ ΕΙΝΑΙ ΣΝ>ΣΗ, ΑΛΛΑ ΜΕ ΜΙΚΡΗ ΔΙΑΦΟΡΑ, ΕΝΩ ΣΤΟ ΒΟΡΕΙΟ ΑΙΓΑΙΟ ΕΙΝΑΙ ΣΝ>>ΣΗ>ΣΗ. ΣΤΗ ΔΥΤΙΚΗ ΕΛΛΑΔΑ ΥΠΟΛΟΓΙΣΘΗΚΕ ΣΥΜΠΙΕΣΤΙΚΗΤΕΚΤΟΝΙΚΗ ΤΑΣΗ 10 ΜΡΑ ΚΑΙ ΣΤΟ ΒΟΡΕΙΟ ΑΙΓΑΙΟ ΕΦΕΛΚΥΣΤΙΚΗΣ 3 ΜΡΑ. ΟΡΙΟΘΕΤΗΘΗΚΑΝ ΕΠΙΣΗΣ ΕΠΑΡΧΙΕΣ ΤΟΥ ΕΝΤΑΤΙΚΟΥ ΠΕΔΙΟΥ ΠΟΥ ΒΡΙΣΚΟΝΤΑΙ ΣΕ ΑΝΤΙΣΤΟΙΧΙΑ ΜΕ ΓΕΩΘΕΡΜΙΚΕΣ ΕΠΑΡΧΙΕΣ. ΜΕΛΕΤΑΤΑΙ Η ΘΕΡΜΙΚΗ ΚΑΤΑΣΤΑΣΗ ΚΑΙ Η ΜΗΧΑΝΙΚΗ ΑΝΤΟΧΗ ΤΗΣ ΛΙΘΟΣΦΑΙΡΑΣ ΣΤΟ ΑΙΓΑΙΟ, ΚΑΘΩΣ ΚΑΙ Η ΘΕΡΜΙΚΗ ΕΞΕΛΙΞΗ ΣΤΗ ΔΥΤΙΚΗ ΕΛΛΑΔΑ. ΣΤΟ ΒΟΡΕΙΟ ΑΙΓΑΙΟ ΥΠΟΛΟΓΙΣΘΗΚΕ Ο ΣΥΝΤΕΛΕΣΤΗΣ ΛΕΠΤΥΝΣΗΣ ΣΤΟ ΦΛΟΙΟ (1,4-1,5) ΚΑΙ ΤΟΝ ΜΑΝΔΥΑ (2,4-9,8). ΕΞΕΤΑΖΕΤΑΙ Ο ΜΗΧΑΝΙΣΜΟΣ ΥΠΟΒΥΘΙΣΗΣ ΤΗΣ ΑΦΡΙΚΑΝΙΚΗΣ ΠΛΑΚΑΣ ΣΕ ΣΧΕΣΗ ΜΕ ΤΟ ΕΝΕΡΓΟ ΕΝΤΑΤΙΚΟ ΠΕΔΙΟ, ΤΗ ΘΕΡΜΙΚΗ ΚΑΤΑΣΤΑΣΗ, ΤΗΝ ΜΕΤΑΝΑΣΤΕΥΣΗ ΗΦΑΙΣΤΕΙΟΤΗΤΟΣ ΑΠΟ ΤΗ ΘΡΑΚΗ ΣΤΟ ΑΙΓΑΙΟ ΚΑΙ ΤΟ ΜΗΧΑΝΙΣΜΟ ΓΕΝΕΣΗΣ ΤΩΝ ΝΕΟΓΕΝΩΝ ΙΖΗΜΑΤΟΓΕΝΩΝ ΛΕΚΑΝΩΝ."]},{"key":"dc:title","label":"Title","values":["ΘΕΡΜΟΜΗΧΑΝΙΚΗ ΣΥΜΠΕΡΙΦΟΡΑ ΤΗΣ ΛΙΘΟΣΦΑΙΡΑΣ ΣΤΟΝ ΕΛΛΗΝΙΚΟ ΧΩΡΟ","THERMOMECHANICAL BEHAVIOUR OF THE LITHOSPHERE IN GREECE"]}]}],"canonical_facts":{"dc:creator":["Χιώτης, Ευστάθιος"],"dc:date":["1990"],"dc:description":["A QUANTITATIVE STUDY OF BOTH THE THERMAL AND MECHANICAL STATE OF THE LITHOSPHERE IN GREECE AND THEIR INTERRELATIONSHIP IN THE COURSE OF THE GEOLOGIC TIME. THEMAIN DATA USED ARE NEOTECTONIC ONES, ABSOLUTE VALUES OF THE EFFECTIVE PRINCIPAL STRESSES MEASURED THROUGH HYDROFRACTURING IN OIL WELLS, THE TECTONIC SUBSIDENCE OF NEOGENE SEDIMENTARY BASINS, TEMPERATURE MEASUREMENTS AND ESTIMATED HEAT FLOW, PALEOGEOTHERMAL INDICATORS, DEEP GEOPHYSICAL DATA RELATED TO THE CRUST STRUCTURE, RHEOLOGICAL MODELS FOR THE STRENGTH OF THE LITHOSPHERE. OFFSHORE AND WEST OF PARGA THE VERTICAL PRINCIPAL STRESS (ΣΝ) IS INTERMEDIATE BETWEEN ΣΗ AND ΣΗ, IN NW PELOPONNESE ΣΝ EXCEEDS ΣΗ WITH A SLIGHT DIFFERENCY ONLY, WHEREAS IT ISΣΝ>>ΣΗ>ΣΗ IN THE NORTH AEGEAN. A COMPRESSIVE TECTONIC STRESS OF ABOUT 10 MPA IS ESTIMATED FOR WESTERN GREECE, IN CONTRAST WITH AN EXTENSIVE STRESS OF ABOUT 3MPA IN THE NORTH AEGEAN. TECTONICS PROVINCES WERE DELINIATED IN CLOSE CORRESPONDENCE TO GEOTHERMAL PROVINCES. THE THERMAL STATE AND THE MECHANICAL STRENGTH OF THE AEGEAN LITHOSPHERE WAS STUDIED, AS WELL AS THE THERMAL HISTORY OF WESTERNGREECE. A THINNING FACTOR OF 1,4-1,5 IS ESTIMATED FOR THE NORTH AEGEAN CRUST AND 2,4-9,8 FOR THE MANTTLE. A MODEL OF SUBDUCTION OF THE AFRICAN LITHOSPHERE ISEXAMINED IN RELATIONSHIP TO THE ACTIVE STRESS FIELD, THE THERMAL STATE, THE MIGRATION OF VOLCANISM FROM THRACE TO THE PRESENT POSITION IN THE AEGEAN AND THE FORMATION OF NEOGENE BASINS AND TROUGHS.","ΠΟΣΟΤΙΚΗ ΜΕΛΕΤΗ ΤΗΣ ΘΕΡΜΙΚΗΣ ΚΑΙ ΤΗΣ ΜΗΧΑΝΙΚΗΣ ΚΑΤΑΣΤΑΣΗΣ ΤΗΣ ΛΙΘΟΣΦΑΙΡΑΣ ΣΤΟΝ ΕΛΛΗΝΙΚΟ ΧΩΡΟ ΚΑΙ ΤΗΣ ΜΕΤΑΞΥ ΤΟΥΣ ΣΧΕΣΕΩΣ ΣΤΗ ΔΙΑΡΚΕΙΑ ΤΟΥ ΓΕΩΛΟΓΙΚΟΥ ΧΡΟΝΟΥ. ΤΑ ΚΥΡΙΑ ΣΤΟΙΧΕΙΑ ΠΟΥ ΧΡΗΣΙΜΟΠΟΙΟΥΝΤΑΙ ΕΙΝΑΙ ΝΕΟΤΕΚΤΟΝΙΚΑ, ΑΠΟΛΥΤΕΣ ΤΙΜΕΣ ΤΩΝ ΕΝΕΡΓΩΝ ΚΥΡΙΩΝ ΤΑΣΕΩΝ ΥΠΟΛΟΓΙΣΜΕΝΕΣ ΑΠΟ ΔΕΔΟΜΕΝΑ ΥΔΡΟΡΩΓΜΑΤΩΣΗΣ ΣΕ ΓΕΩΤΡΗΣΕΙΣ ΠΕΤΡΕΛΑΙΟΥ, Η ΤΕΚΤΟΝΙΚΗ ΣΥΝΙΖΗΣΗ ΝΕΟΓΕΝΩΝ ΙΖΗΜΑΤΟΓΕΝΩΝ ΛΕΚΑΝΩΝ, ΜΕΤΡΗΣΕΙΣ ΘΕΡΜΟΚΡΑΣΙΑΣ ΚΑΙ ΕΚΤΙΜΗΣΕΙΣ ΤΗΣ ΡΟΗΣ ΘΕΡΜΟΤΗΤΟΣ, ΠΑΛΑΙΟΘΕΡΜΙΚΟΙ ΔΕΙΚΤΕΣ, ΓΕΩΦΥΣΙΚΑ ΔΕΔΟΜΕΝΑ ΓΙΑ ΤΗ ΔΟΜΗ ΤΟΥ ΦΛΟΙΟΥ, ΠΡΟΤΥΠΑ ΥΠΟΛΟΓΙΣΜΟΥ ΤΗΣ ΑΝΤΟΧΗΣ ΤΗΣ ΛΙΘΟΣΦΑΙΡΑΣ. ΣΤΗ ΘΑΛΑΣΣΙΑ ΠΕΡΙΟΧΗ ΔΥΤΙΚΑ ΤΗΣ ΠΑΡΓΑΣ Η ΚΑΤΑΚΟΡΥΦΗ ΚΥΡΙΑ ΤΑΣΗ (ΣΝ) ΕΙΝΑΙ ΕΝΔΙΑΜΕΣΗ ΜΕΤΑΞΥ ΣΗ ΚΑΙ ΣΗ, ΣΤΗ ΒΔ ΠΕΛΟΠΟΝΝΗΣΟ ΕΙΝΑΙ ΣΝ>ΣΗ, ΑΛΛΑ ΜΕ ΜΙΚΡΗ ΔΙΑΦΟΡΑ, ΕΝΩ ΣΤΟ ΒΟΡΕΙΟ ΑΙΓΑΙΟ ΕΙΝΑΙ ΣΝ>>ΣΗ>ΣΗ. ΣΤΗ ΔΥΤΙΚΗ ΕΛΛΑΔΑ ΥΠΟΛΟΓΙΣΘΗΚΕ ΣΥΜΠΙΕΣΤΙΚΗΤΕΚΤΟΝΙΚΗ ΤΑΣΗ 10 ΜΡΑ ΚΑΙ ΣΤΟ ΒΟΡΕΙΟ ΑΙΓΑΙΟ ΕΦΕΛΚΥΣΤΙΚΗΣ 3 ΜΡΑ. ΟΡΙΟΘΕΤΗΘΗΚΑΝ ΕΠΙΣΗΣ ΕΠΑΡΧΙΕΣ ΤΟΥ ΕΝΤΑΤΙΚΟΥ ΠΕΔΙΟΥ ΠΟΥ ΒΡΙΣΚΟΝΤΑΙ ΣΕ ΑΝΤΙΣΤΟΙΧΙΑ ΜΕ ΓΕΩΘΕΡΜΙΚΕΣ ΕΠΑΡΧΙΕΣ. ΜΕΛΕΤΑΤΑΙ Η ΘΕΡΜΙΚΗ ΚΑΤΑΣΤΑΣΗ ΚΑΙ Η ΜΗΧΑΝΙΚΗ ΑΝΤΟΧΗ ΤΗΣ ΛΙΘΟΣΦΑΙΡΑΣ ΣΤΟ ΑΙΓΑΙΟ, ΚΑΘΩΣ ΚΑΙ Η ΘΕΡΜΙΚΗ ΕΞΕΛΙΞΗ ΣΤΗ ΔΥΤΙΚΗ ΕΛΛΑΔΑ. ΣΤΟ ΒΟΡΕΙΟ ΑΙΓΑΙΟ ΥΠΟΛΟΓΙΣΘΗΚΕ Ο ΣΥΝΤΕΛΕΣΤΗΣ ΛΕΠΤΥΝΣΗΣ ΣΤΟ ΦΛΟΙΟ (1,4-1,5) ΚΑΙ ΤΟΝ ΜΑΝΔΥΑ (2,4-9,8). ΕΞΕΤΑΖΕΤΑΙ Ο ΜΗΧΑΝΙΣΜΟΣ ΥΠΟΒΥΘΙΣΗΣ ΤΗΣ ΑΦΡΙΚΑΝΙΚΗΣ ΠΛΑΚΑΣ ΣΕ ΣΧΕΣΗ ΜΕ ΤΟ ΕΝΕΡΓΟ ΕΝΤΑΤΙΚΟ ΠΕΔΙΟ, ΤΗ ΘΕΡΜΙΚΗ ΚΑΤΑΣΤΑΣΗ, ΤΗΝ ΜΕΤΑΝΑΣΤΕΥΣΗ ΗΦΑΙΣΤΕΙΟΤΗΤΟΣ ΑΠΟ ΤΗ ΘΡΑΚΗ ΣΤΟ ΑΙΓΑΙΟ ΚΑΙ ΤΟ ΜΗΧΑΝΙΣΜΟ ΓΕΝΕΣΗΣ ΤΩΝ ΝΕΟΓΕΝΩΝ ΙΖΗΜΑΤΟΓΕΝΩΝ ΛΕΚΑΝΩΝ."],"dc:identifier":["10.12681/eadd/1268","http://hdl.handle.net/10442/hedi/1268"],"dc:language":["gre"],"dc:publisher":["Εθνικό Μετσόβιο Πολυτεχνείο (ΕΜΠ)","National Technical University of Athens (NTUA)"],"dc:subject":["Aegean sea","GEOTHERM","HYDROFRACTURING","Oil generation","Pore pressure","REACTIVATION OF FAULTS","SEBDUCTION MODEL IN AEGEAN","STRENGTH OF THE LITHOSPHERE","Stress field","Αιγαίο","ΑΝΑΔΡΑΣΗ ΡΗΓΜΑΤΩΝ","ΑΝΤΟΧΗ ΛΙΘΟΣΦΑΙΡΑΣ","ΑΝΤΟΧΗ ΡΗΓΜΑΤΩΝ","ΓΕΩΘΕΡΜΟΣ","ΕΝΤΑΤΙΚΟ ΠΕΔΙΟ","Πετρελαιογένεση","Πίεση πόρων","ΠΡΟΤΥΠΟ ΥΠΟΒΥΘΙΣΗΣ ΣΤΟ ΑΙΓΑΙΟ","ΣΧΗΜΑΤΙΣΜΟΣ ΙΖΗΜΑΤΟΓΕΝΩΝ ΤΑΦΡΩΝ","ΥΔΡΟΡΩΓΜΑΤΩΣΗ","Engineering and Technology","Environmental Engineering","Επιστήμες Μηχανικού και Τεχνολογία","Περιβαλλοντική Μηχανική"],"dc:title":["ΘΕΡΜΟΜΗΧΑΝΙΚΗ ΣΥΜΠΕΡΙΦΟΡΑ ΤΗΣ ΛΙΘΟΣΦΑΙΡΑΣ ΣΤΟΝ ΕΛΛΗΝΙΚΟ ΧΩΡΟ","THERMOMECHANICAL BEHAVIOUR OF THE LITHOSPHERE IN GREECE"],"dc:type":["PhD Thesis"]},"updated_at":"2026-07-24T02:24:49Z"}