{"id":{"repo_id":"greece","oai_identifier":"oai:10442/0632"},"canonical_url":"https://search.dev.ndltd.org/etd/greece/oai:10442/0632","repository":{"repo_id":"greece","name":"Greek National Archive of PhD Theses","base_url":"https://phdtheses.ekt.gr/eadd_oai/request"},"display":{"title":"ΤΕΧΝΙΚΟΓΕΩΛΟΓΙΚΟΙ ΧΑΡΑΚΤΗΡΕΣ ΤΩΝ ΜΑΡΓΩΝ ΗΡΑΚΛΕΙΟΥ ΚΡΗΤΗΣ","abstract":"IN THIS THESIS, IRAKLION MARLS WHICH CONSTITUTE THE MAIN GEOLOGICAL FORMATION OF THEIR GEOLOGICAL ENVIROMENT IS DESCRIBED AND THEIR MINERALOGICAL COMPOSITION AND FABIRC ARE DETERMINED. FOR THE GEOTECHNICAL DESCRIPTION AND CLASSIFICATION OF THESE MARLS PARTICLE SIZE DISTRIBUTION AND PLASTICITY ARE EXAMINED. CONSEQUENTLY, SOME RESULTS FOR THEIR CLAY PARTICLES AGGREGATION AND THEIR ACTIVITY ARE PRESENTED AND SOME CORRELATIONS OF CALCIUM CARBONATE CONTENT WITH PLASTICITY AND CLAY CONTENT ARE DETERMINED . GEOMECHANICAL CHARACTERISTICS OF THESE MARLS, SUCH AS RESISTANCE TO PENETRATION OF TERZAGHI SAMPLER, UNCONFINED AND TRIAXIAL COMPRESSIVE STRENGTHS, SENSITIVITY AND COMPRESSIBILITY ARE STUDIED AND THE RESULTS ARE COMPARED WITH OTHER FACTORS SUCH AS THE DEPTH OF SAMPLING AND DIAGENESISOF MARLS. SWELLING AND RESIDUAL STRENGTH CHARACTERISTICS ARE STUDIED IN MORE DETAIL AND SOME CORRELATIONS OF THESE WITH THE MINERAL COMPOSITION AND THE PHYSICAL PROPERTIES ARE GIVEN. FINALLY, THE ENGINEERING GEOLOGICAL UNITS OF IRAKLIONCITY, WHICH WERE MAPPED IN A SCALE 1 : 5.000, ARE DESCRIBED AND PRACTICAL APPLICATIONS OF THIS RESEARCH ARE DISCUSSED.","abstract_html":"IN THIS THESIS, IRAKLION MARLS WHICH CONSTITUTE THE MAIN GEOLOGICAL FORMATION OF THEIR GEOLOGICAL ENVIROMENT IS DESCRIBED AND THEIR MINERALOGICAL COMPOSITION AND FABIRC ARE DETERMINED. FOR THE GEOTECHNICAL DESCRIPTION AND CLASSIFICATION OF THESE MARLS PARTICLE SIZE DISTRIBUTION AND PLASTICITY ARE EXAMINED. CONSEQUENTLY, SOME RESULTS FOR THEIR CLAY PARTICLES AGGREGATION AND THEIR ACTIVITY ARE PRESENTED AND SOME CORRELATIONS OF CALCIUM CARBONATE CONTENT WITH PLASTICITY AND CLAY CONTENT ARE DETERMINED . GEOMECHANICAL CHARACTERISTICS OF THESE MARLS, SUCH AS RESISTANCE TO PENETRATION OF TERZAGHI SAMPLER, UNCONFINED AND TRIAXIAL COMPRESSIVE STRENGTHS, SENSITIVITY AND COMPRESSIBILITY ARE STUDIED AND THE RESULTS ARE COMPARED WITH OTHER FACTORS SUCH AS THE DEPTH OF SAMPLING AND DIAGENESISOF MARLS. SWELLING AND RESIDUAL STRENGTH CHARACTERISTICS ARE STUDIED IN MORE DETAIL AND SOME CORRELATIONS OF THESE WITH THE MINERAL COMPOSITION AND THE PHYSICAL PROPERTIES ARE GIVEN. FINALLY, THE ENGINEERING GEOLOGICAL UNITS OF IRAKLIONCITY, WHICH WERE MAPPED IN A SCALE 1 : 5.000, ARE DESCRIBED AND PRACTICAL APPLICATIONS OF THIS RESEARCH ARE DISCUSSED.","abstract_has_math":false,"creators":["Τσιαμπάος, Γεώργιος"],"institution":"Πανεπιστήμιο Πατρών","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":"2026-07-24T02:25:21Z","subjects":["Engineering geology","LABORATORY TESTS","Mapping","Marl","Mechanical properties","Mineralogy","Physical properties","RESIDUAL SHEAR STRENTH","SITE INVESTIGATION","Swelling","Διόγκωση","ΕΡΓΑΣΤΗΡΙΑΚΕΣ ΔΟΚΙΜΕΣ","Έρευνα πεδίου","Μάργα","Μηχανικά χαρακτηριστικά","Ορυκτολογικές αναλύσεις","ΠΑΡΑΜΕΝΟΥΣΑ ΔΙΑΤΜΗΤΙΚΗ ΑΝΤΟΧΗ","Τεχνική γεωλογία","Φυσικά χαρακτηριστικά","Χαρτογράφηση","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/0632"],"render_values":[{"text":"10.12681/eadd/0632","href":"https://doi.org/10.12681/eadd/0632","code":true}]}]},"links":{"outbound_url":"http://hdl.handle.net/10442/hedi/0632","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:creator","label":"Author","values":["Τσιαμπάος, Γεώργιος"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["1988"]},{"key":"dc:publisher","label":"Institution","values":["Πανεπιστήμιο Πατρών","University of Patras"]},{"key":"dc:type","label":"Dc Type","values":["PhD Thesis"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["Engineering geology","LABORATORY TESTS","Mapping","Marl","Mechanical properties","Mineralogy","Physical properties","RESIDUAL SHEAR STRENTH","SITE INVESTIGATION","Swelling","Διόγκωση","ΕΡΓΑΣΤΗΡΙΑΚΕΣ ΔΟΚΙΜΕΣ","Έρευνα πεδίου","Μάργα","Μηχανικά χαρακτηριστικά","Ορυκτολογικές αναλύσεις","ΠΑΡΑΜΕΝΟΥΣΑ ΔΙΑΤΜΗΤΙΚΗ ΑΝΤΟΧΗ","Τεχνική γεωλογία","Φυσικά χαρακτηριστικά","Χαρτογράφηση","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/0632","http://hdl.handle.net/10442/hedi/0632"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["IN THIS THESIS, IRAKLION MARLS WHICH CONSTITUTE THE MAIN GEOLOGICAL FORMATION OF THEIR GEOLOGICAL ENVIROMENT IS DESCRIBED AND THEIR MINERALOGICAL COMPOSITION AND FABIRC ARE DETERMINED. FOR THE GEOTECHNICAL DESCRIPTION AND CLASSIFICATION OF THESE MARLS PARTICLE SIZE DISTRIBUTION AND PLASTICITY ARE EXAMINED. CONSEQUENTLY, SOME RESULTS FOR THEIR CLAY PARTICLES AGGREGATION AND THEIR ACTIVITY ARE PRESENTED AND SOME CORRELATIONS OF CALCIUM CARBONATE CONTENT WITH PLASTICITY AND CLAY CONTENT ARE DETERMINED . GEOMECHANICAL CHARACTERISTICS OF THESE MARLS, SUCH AS RESISTANCE TO PENETRATION OF TERZAGHI SAMPLER, UNCONFINED AND TRIAXIAL COMPRESSIVE STRENGTHS, SENSITIVITY AND COMPRESSIBILITY ARE STUDIED AND THE RESULTS ARE COMPARED WITH OTHER FACTORS SUCH AS THE DEPTH OF SAMPLING AND DIAGENESISOF MARLS. SWELLING AND RESIDUAL STRENGTH CHARACTERISTICS ARE STUDIED IN MORE DETAIL AND SOME CORRELATIONS OF THESE WITH THE MINERAL COMPOSITION AND THE PHYSICAL PROPERTIES ARE GIVEN. FINALLY, THE ENGINEERING GEOLOGICAL UNITS OF IRAKLIONCITY, WHICH WERE MAPPED IN A SCALE 1 : 5.000, ARE DESCRIBED AND PRACTICAL APPLICATIONS OF THIS RESEARCH ARE DISCUSSED.","ΣΤΗΝ ΠΑΡΟΥΣΑ ΔΙΑΤΡΙΒΗ, ΕΞΕΤΑΖΟΝΤΑΙ ΟΙ ΜΑΡΓΕΣ ΤΟΥ ΗΡΑΚΛΕΙΟΥ ΚΡΗΤΗΣ ΠΟΥ ΑΠΟΤΕΛΟΥΝΤΟΝ ΚΥΡΙΟ ΓΕΩΛΟΓΙΚΟ ΣΧΗΜΑΤΙΣΜΟ ΤΗΣ ΠΟΛΗΣ. ΠΕΡΙΓΡΑΦΕΤΑΙ ΤΟ ΓΕΩΛΟΓΙΚΟ ΤΟΥΣ ΠΕΡΙΒΑΛΛΟΝ ΚΑΙ ΠΡΟΣΔΙΟΡΙΖΕΤΑΙ Η ΟΡΥΚΤΟΛΟΓΙΚΗ ΣΥΣΤΑΣΗ ΚΑΙ Ο ΙΣΤΟΣ ΤΟΥΣ. ΓΙΑ ΤΗ ΓΕΩΤΕΧΝΙΚΗ ΠΕΡΙΓΡΑΦΗ ΚΑΙ ΤΑΞΙΝΟΜΗΣΗ ΤΩΝ ΜΑΡΓΩΝ ΑΥΤΩΝ ΕΞΕΤΑΖΟΝΤΑΙ Η ΚΟΚΚΟΜΕΤΡΙΚΗ ΔΙΑΒΑΘΜΙΣΗ ΚΑΙ Η ΠΛΑΣΤΙΚΟΤΗΤΑ ΤΟΥΣ, ΚΑΙ ΣΥΝΑΓΟΝΤΑΙ ΣΥΜΠΕΡΑΣΜΑΤΑ ΤΟΣΟ ΓΙΑ ΤΗΝ ΣΥΣΣΩΜΑΤΩΣΗ ΤΩΝ ΑΡΓΙΛΙΚΩΝ ΣΩΜΑΤΙΔΙΩΝ ΟΣΟ ΚΑΙ ΓΙΑ ΤΗΝ ΕΝΕΡΓΟΤΗΤΑ ΤΟΥΣ. ΙΔΙΑΙΤΕΡΗ ΕΜΦΑΣΗΔΙΝΕΤΑΙ ΣΤΟ ΣΥΣΧΕΤΙΣΜΟ ΤΟΥ ΠΟΣΟΣΤΟΥ ΤΟΥ ΑΝΘΡΑΚΙΚΟΥ ΑΣΒΕΣΤΙΟΥ ΜΕ ΤΗΝ ΠΛΑΣΤΙΚΟΤΗΤΑ ΚΑΙ ΤΟ ΠΟΣΟΣΤΟ ΤΟΥ ΑΡΓΙΛΙΚΟΥ ΚΛΑΣΜΑΤΟΣ. ΑΠΟ ΤΟΥΣ ΓΕΩΜΗΧΑΝΙΚΟΥΣ ΧΑΡΑΚΤΗΡΕΣ ΤΩΝ ΜΑΡΓΩΝ ΠΡΟΣΔΙΟΡΙΖΟΝΤΑΙ Η ΑΝΤΙΣΤΑΣΗ ΤΟΥΣ ΣΤΗ ΔΙΕΙΣΔΥΣΗ ΤΟΥ ΔΕΙΓΜΑΤΟΛΗΠΤΗ TERZAGHI, Η ΑΝΤΟΧΗ ΤΟΥΣ ΣΕ ΑΝΕΜΠΟΔΙΣΤΗ ΚΑΙ ΤΡΙΑΞΟΝΙΚΗ ΘΛΙΨΗ, Η ΕΥΑΙΣΘΗΣΙΑ ΤΟΥΣ ΚΑΙ ΗΣΥΜΠΙΕΣΤΟΤΗΤΑ ΤΟΥΣ, ΠΟΥ ΣΧΕΤΙΖΟΝΤΑΙ ΜΕ ΑΛΛΟΥΣ ΠΑΡΑΓΟΝΤΕΣ ΟΠΩΣ ΤΟ ΒΑΘΟΣ ΔΕΙΓΜΑΤΟΛΗΨΙΑΣ ΚΑΙ Η ΔΙΑΓΕΝΕΣΗ ΤΟΥΣ. Η ΔΙΟΓΚΩΣΙΜΟΤΗΤΑ ΚΑΙ Η ΠΑΡΑΜΕΝΟΥΣΑ ΔΙΑΤΜΗΤΙΚΗ ΑΝΤΟΧΗ ΤΩΝ ΜΑΡΓΩΝ ΜΕΛΕΤΩΝΤΑΙ ΛΕΠΤΟΜΕΡΕΣΤΕΡΑ ΚΑΙ ΣΥΣΧΕΤΙΖΟΝΤΑΙ ΜΕ ΤΗΝ ΟΡΥΚΤΟΛΟΓΙΚΗ ΣΥΣΤΑΣΗ ΚΑΙ ΤΑ ΦΥΣΙΚΑ ΧΑΡΑΚΤΗΡΙΣΤΙΚΑ ΤΟΥΣ. ΤΕΛΟΣ, ΠΕΡΙΓΡΑΦΟΝΤΑΙ ΟΙ ΤΕΧΝΙΚΟΓΕΩΛΟΓΙΚΟΙ ΧΑΡΑΚΤΗΡΕΣ ΤΩΝ ΕΝΟΤΗΤΩΝ ΠΟΥ ΧΑΡΤΟΓΡΑΦΗΘΗΚΑΝ ΣΤΗΝ ΠΟΛΗ ΤΟΥ ΗΡΑΚΛΕΙΟΥ ΣΕ ΚΛΙΜΑΚΑ 1 : 5.ΟΟΟ, ΚΑΙ ΑΝΑΦΕΡΟΝΤΑΙ ΟΙ ΠΡΑΚΤΙΚΕΣ ΕΦΑΡΜΟΓΕΣ ΤΗΣ ΕΡΕΥΝΑΣ ΑΥΤΗΣ."]},{"key":"dc:title","label":"Title","values":["ΤΕΧΝΙΚΟΓΕΩΛΟΓΙΚΟΙ ΧΑΡΑΚΤΗΡΕΣ ΤΩΝ ΜΑΡΓΩΝ ΗΡΑΚΛΕΙΟΥ ΚΡΗΤΗΣ","ENGINEERING GEOLOGICAL CHARACTERS OF IRAKLION MARLS"]}]}],"canonical_facts":{"dc:creator":["Τσιαμπάος, Γεώργιος"],"dc:date":["1988"],"dc:description":["IN THIS THESIS, IRAKLION MARLS WHICH CONSTITUTE THE MAIN GEOLOGICAL FORMATION OF THEIR GEOLOGICAL ENVIROMENT IS DESCRIBED AND THEIR MINERALOGICAL COMPOSITION AND FABIRC ARE DETERMINED. FOR THE GEOTECHNICAL DESCRIPTION AND CLASSIFICATION OF THESE MARLS PARTICLE SIZE DISTRIBUTION AND PLASTICITY ARE EXAMINED. CONSEQUENTLY, SOME RESULTS FOR THEIR CLAY PARTICLES AGGREGATION AND THEIR ACTIVITY ARE PRESENTED AND SOME CORRELATIONS OF CALCIUM CARBONATE CONTENT WITH PLASTICITY AND CLAY CONTENT ARE DETERMINED . GEOMECHANICAL CHARACTERISTICS OF THESE MARLS, SUCH AS RESISTANCE TO PENETRATION OF TERZAGHI SAMPLER, UNCONFINED AND TRIAXIAL COMPRESSIVE STRENGTHS, SENSITIVITY AND COMPRESSIBILITY ARE STUDIED AND THE RESULTS ARE COMPARED WITH OTHER FACTORS SUCH AS THE DEPTH OF SAMPLING AND DIAGENESISOF MARLS. SWELLING AND RESIDUAL STRENGTH CHARACTERISTICS ARE STUDIED IN MORE DETAIL AND SOME CORRELATIONS OF THESE WITH THE MINERAL COMPOSITION AND THE PHYSICAL PROPERTIES ARE GIVEN. FINALLY, THE ENGINEERING GEOLOGICAL UNITS OF IRAKLIONCITY, WHICH WERE MAPPED IN A SCALE 1 : 5.000, ARE DESCRIBED AND PRACTICAL APPLICATIONS OF THIS RESEARCH ARE DISCUSSED.","ΣΤΗΝ ΠΑΡΟΥΣΑ ΔΙΑΤΡΙΒΗ, ΕΞΕΤΑΖΟΝΤΑΙ ΟΙ ΜΑΡΓΕΣ ΤΟΥ ΗΡΑΚΛΕΙΟΥ ΚΡΗΤΗΣ ΠΟΥ ΑΠΟΤΕΛΟΥΝΤΟΝ ΚΥΡΙΟ ΓΕΩΛΟΓΙΚΟ ΣΧΗΜΑΤΙΣΜΟ ΤΗΣ ΠΟΛΗΣ. ΠΕΡΙΓΡΑΦΕΤΑΙ ΤΟ ΓΕΩΛΟΓΙΚΟ ΤΟΥΣ ΠΕΡΙΒΑΛΛΟΝ ΚΑΙ ΠΡΟΣΔΙΟΡΙΖΕΤΑΙ Η ΟΡΥΚΤΟΛΟΓΙΚΗ ΣΥΣΤΑΣΗ ΚΑΙ Ο ΙΣΤΟΣ ΤΟΥΣ. ΓΙΑ ΤΗ ΓΕΩΤΕΧΝΙΚΗ ΠΕΡΙΓΡΑΦΗ ΚΑΙ ΤΑΞΙΝΟΜΗΣΗ ΤΩΝ ΜΑΡΓΩΝ ΑΥΤΩΝ ΕΞΕΤΑΖΟΝΤΑΙ Η ΚΟΚΚΟΜΕΤΡΙΚΗ ΔΙΑΒΑΘΜΙΣΗ ΚΑΙ Η ΠΛΑΣΤΙΚΟΤΗΤΑ ΤΟΥΣ, ΚΑΙ ΣΥΝΑΓΟΝΤΑΙ ΣΥΜΠΕΡΑΣΜΑΤΑ ΤΟΣΟ ΓΙΑ ΤΗΝ ΣΥΣΣΩΜΑΤΩΣΗ ΤΩΝ ΑΡΓΙΛΙΚΩΝ ΣΩΜΑΤΙΔΙΩΝ ΟΣΟ ΚΑΙ ΓΙΑ ΤΗΝ ΕΝΕΡΓΟΤΗΤΑ ΤΟΥΣ. ΙΔΙΑΙΤΕΡΗ ΕΜΦΑΣΗΔΙΝΕΤΑΙ ΣΤΟ ΣΥΣΧΕΤΙΣΜΟ ΤΟΥ ΠΟΣΟΣΤΟΥ ΤΟΥ ΑΝΘΡΑΚΙΚΟΥ ΑΣΒΕΣΤΙΟΥ ΜΕ ΤΗΝ ΠΛΑΣΤΙΚΟΤΗΤΑ ΚΑΙ ΤΟ ΠΟΣΟΣΤΟ ΤΟΥ ΑΡΓΙΛΙΚΟΥ ΚΛΑΣΜΑΤΟΣ. ΑΠΟ ΤΟΥΣ ΓΕΩΜΗΧΑΝΙΚΟΥΣ ΧΑΡΑΚΤΗΡΕΣ ΤΩΝ ΜΑΡΓΩΝ ΠΡΟΣΔΙΟΡΙΖΟΝΤΑΙ Η ΑΝΤΙΣΤΑΣΗ ΤΟΥΣ ΣΤΗ ΔΙΕΙΣΔΥΣΗ ΤΟΥ ΔΕΙΓΜΑΤΟΛΗΠΤΗ TERZAGHI, Η ΑΝΤΟΧΗ ΤΟΥΣ ΣΕ ΑΝΕΜΠΟΔΙΣΤΗ ΚΑΙ ΤΡΙΑΞΟΝΙΚΗ ΘΛΙΨΗ, Η ΕΥΑΙΣΘΗΣΙΑ ΤΟΥΣ ΚΑΙ ΗΣΥΜΠΙΕΣΤΟΤΗΤΑ ΤΟΥΣ, ΠΟΥ ΣΧΕΤΙΖΟΝΤΑΙ ΜΕ ΑΛΛΟΥΣ ΠΑΡΑΓΟΝΤΕΣ ΟΠΩΣ ΤΟ ΒΑΘΟΣ ΔΕΙΓΜΑΤΟΛΗΨΙΑΣ ΚΑΙ Η ΔΙΑΓΕΝΕΣΗ ΤΟΥΣ. Η ΔΙΟΓΚΩΣΙΜΟΤΗΤΑ ΚΑΙ Η ΠΑΡΑΜΕΝΟΥΣΑ ΔΙΑΤΜΗΤΙΚΗ ΑΝΤΟΧΗ ΤΩΝ ΜΑΡΓΩΝ ΜΕΛΕΤΩΝΤΑΙ ΛΕΠΤΟΜΕΡΕΣΤΕΡΑ ΚΑΙ ΣΥΣΧΕΤΙΖΟΝΤΑΙ ΜΕ ΤΗΝ ΟΡΥΚΤΟΛΟΓΙΚΗ ΣΥΣΤΑΣΗ ΚΑΙ ΤΑ ΦΥΣΙΚΑ ΧΑΡΑΚΤΗΡΙΣΤΙΚΑ ΤΟΥΣ. ΤΕΛΟΣ, ΠΕΡΙΓΡΑΦΟΝΤΑΙ ΟΙ ΤΕΧΝΙΚΟΓΕΩΛΟΓΙΚΟΙ ΧΑΡΑΚΤΗΡΕΣ ΤΩΝ ΕΝΟΤΗΤΩΝ ΠΟΥ ΧΑΡΤΟΓΡΑΦΗΘΗΚΑΝ ΣΤΗΝ ΠΟΛΗ ΤΟΥ ΗΡΑΚΛΕΙΟΥ ΣΕ ΚΛΙΜΑΚΑ 1 : 5.ΟΟΟ, ΚΑΙ ΑΝΑΦΕΡΟΝΤΑΙ ΟΙ ΠΡΑΚΤΙΚΕΣ ΕΦΑΡΜΟΓΕΣ ΤΗΣ ΕΡΕΥΝΑΣ ΑΥΤΗΣ."],"dc:identifier":["10.12681/eadd/0632","http://hdl.handle.net/10442/hedi/0632"],"dc:language":["gre"],"dc:publisher":["Πανεπιστήμιο Πατρών","University of Patras"],"dc:subject":["Engineering geology","LABORATORY TESTS","Mapping","Marl","Mechanical properties","Mineralogy","Physical properties","RESIDUAL SHEAR STRENTH","SITE INVESTIGATION","Swelling","Διόγκωση","ΕΡΓΑΣΤΗΡΙΑΚΕΣ ΔΟΚΙΜΕΣ","Έρευνα πεδίου","Μάργα","Μηχανικά χαρακτηριστικά","Ορυκτολογικές αναλύσεις","ΠΑΡΑΜΕΝΟΥΣΑ ΔΙΑΤΜΗΤΙΚΗ ΑΝΤΟΧΗ","Τεχνική γεωλογία","Φυσικά χαρακτηριστικά","Χαρτογράφηση","Φυσικές Επιστήμες","Natural Sciences","Γεωεπιστήμες και Επιστήμες Περιβάλλοντος","Earth and Related Environmental Sciences"],"dc:title":["ΤΕΧΝΙΚΟΓΕΩΛΟΓΙΚΟΙ ΧΑΡΑΚΤΗΡΕΣ ΤΩΝ ΜΑΡΓΩΝ ΗΡΑΚΛΕΙΟΥ ΚΡΗΤΗΣ","ENGINEERING GEOLOGICAL CHARACTERS OF IRAKLION MARLS"],"dc:type":["PhD Thesis"]},"updated_at":"2026-07-24T02:25:21Z"}