{"id":{"repo_id":"greece","oai_identifier":"oai:10442/1202"},"canonical_url":"https://search.dev.ndltd.org/etd/greece/oai:10442/1202","repository":{"repo_id":"greece","name":"Greek National Archive of PhD Theses","base_url":"https://phdtheses.ekt.gr/eadd_oai/request"},"display":{"title":"ΤΕΧΝΙΚΟΓΕΩΛΟΓΙΚΕΣ ΣΥΝΘΗΚΕΣ ΣΤΟ ΝΟΜΟ ΑΧΑΙΑΣ-ΓΕΩΜΗΧΑΝΙΚΟΙ ΧΑΡΑΚΤΗΡΕΣ ΤΩΝ ΠΛΕΙΟΠΛΕΙΣΤΟΚΑΙΝΙΚΩΝ ΙΖΗΜΑΤΩΝ","abstract":"THE ENGINEERING-GEOLOGICAL FRAME OF ACHAIA PROVINCE IS GIVEN AT FIRST, BY EVALUATING THE PREDOMINANT CONDITIONS, AND BY DRAWING THE ENGINEERING-GEOLOGICAL MAPOF THE AREA AT A SCALE OF 1:100. 000. IN THIS MAP, 18 LITHOLOGICAL UNITIES AREDISTINGUISHED. FOLLOWING, THE LITHOSTRATIGRAPHY, TECTONICS, MINERALOGICAL COMPOSITION AND FABRIC, AND PHYSICAL AND MECHANICAL PROPERTIES OF THE PLIO-PLEISTOCENE SEDIMENTS FROM THE THREE SEDIMENTATION BASINS (CORINTHIAN, PATRAIKOS AND LEONDION) WERE STUDIED. (SHORTENED)","abstract_html":"THE ENGINEERING-GEOLOGICAL FRAME OF ACHAIA PROVINCE IS GIVEN AT FIRST, BY EVALUATING THE PREDOMINANT CONDITIONS, AND BY DRAWING THE ENGINEERING-GEOLOGICAL MAPOF THE AREA AT A SCALE OF 1:100. 000. IN THIS MAP, 18 LITHOLOGICAL UNITIES AREDISTINGUISHED. FOLLOWING, THE LITHOSTRATIGRAPHY, TECTONICS, MINERALOGICAL COMPOSITION AND FABRIC, AND PHYSICAL AND MECHANICAL PROPERTIES OF THE PLIO-PLEISTOCENE SEDIMENTS FROM THE THREE SEDIMENTATION BASINS (CORINTHIAN, PATRAIKOS AND LEONDION) WERE STUDIED. (SHORTENED)","abstract_has_math":false,"creators":["Ρόζος, Δημήτριος"],"institution":"University of Patras","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":"2026-07-24T02:24:46Z","subjects":["DIFFERENTIAL THERMAL ANALYSIS (D.T.A.)","ELECTRON SCAN MICROSCOPY","Engineering - geological conditions","GEOMECHANICAL CHARACTERS","GEOTECTONIC STRUCTURES","Physical characteristics","PLIO-PLEISTOCENE SEDIMENTS","SLAKE-DURABILITY","SLOPE MOVEMENTS","X-ray diffraction","ΓΕΩΤΕΚΤΟΝΙΚΕΣ ΔΟΜΕΣ","Διαβρωσιμότητα","ΔΙΑΦΟΡΙΚΗ ΘΕΡΜΙΚΗ ΑΝΑΛΥΣΗ (D.T.A.)","ΗΛΕΚΤΡΟΝΙΚΗ ΜΙΚΡΟΑΝΑΛΥΣΗ","ΚΙΝΗΣΕΙΣ ΠΡΑΝΩΝ","Περιθλασιμετρία ακτίνων - Χ","ΠΛΕΙΟΠΛΕΙΣΤΟΚΑΙΝΙΚΑ ΙΖΗΜΑΤΑ","Τεχνικογεωλογικές συνθήκες","ΦΥΣΙΚΕΣ ΙΔΙΟΤΗΤΕΣ-ΓΕΩΜΗΧΑΝΙΚΟΙ ΧΑΡΑΚΤΗΡΕΣ"],"languages":["gre"],"rights":[],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier","label":"Identifier","values":["10.12681/eadd/1202"],"render_values":[{"text":"10.12681/eadd/1202","href":"https://doi.org/10.12681/eadd/1202","code":true}]}]},"links":{"outbound_url":"http://hdl.handle.net/10442/hedi/1202","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:creator","label":"Author","values":["Ρόζος, Δημήτριος"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["1989"]},{"key":"dc:publisher","label":"Institution","values":["University of Patras","Πανεπιστήμιο Πατρών"]},{"key":"dc:type","label":"Dc Type","values":["PhD Thesis"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["DIFFERENTIAL THERMAL ANALYSIS (D.T.A.)","ELECTRON SCAN MICROSCOPY","Engineering - geological conditions","GEOMECHANICAL CHARACTERS","GEOTECTONIC STRUCTURES","Physical characteristics","PLIO-PLEISTOCENE SEDIMENTS","SLAKE-DURABILITY","SLOPE MOVEMENTS","X-ray diffraction","ΓΕΩΤΕΚΤΟΝΙΚΕΣ ΔΟΜΕΣ","Διαβρωσιμότητα","ΔΙΑΦΟΡΙΚΗ ΘΕΡΜΙΚΗ ΑΝΑΛΥΣΗ (D.T.A.)","ΗΛΕΚΤΡΟΝΙΚΗ ΜΙΚΡΟΑΝΑΛΥΣΗ","ΚΙΝΗΣΕΙΣ ΠΡΑΝΩΝ","Περιθλασιμετρία ακτίνων - Χ","ΠΛΕΙΟΠΛΕΙΣΤΟΚΑΙΝΙΚΑ ΙΖΗΜΑΤΑ","Τεχνικογεωλογικές συνθήκες","ΦΥΣΙΚΕΣ ΙΔΙΟΤΗΤΕΣ-ΓΕΩΜΗΧΑΝΙΚΟΙ ΧΑΡΑΚΤΗΡΕΣ"]}]},{"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/1202","http://hdl.handle.net/10442/hedi/1202"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["THE ENGINEERING-GEOLOGICAL FRAME OF ACHAIA PROVINCE IS GIVEN AT FIRST, BY EVALUATING THE PREDOMINANT CONDITIONS, AND BY DRAWING THE ENGINEERING-GEOLOGICAL MAPOF THE AREA AT A SCALE OF 1:100. 000. IN THIS MAP, 18 LITHOLOGICAL UNITIES AREDISTINGUISHED. FOLLOWING, THE LITHOSTRATIGRAPHY, TECTONICS, MINERALOGICAL COMPOSITION AND FABRIC, AND PHYSICAL AND MECHANICAL PROPERTIES OF THE PLIO-PLEISTOCENE SEDIMENTS FROM THE THREE SEDIMENTATION BASINS (CORINTHIAN, PATRAIKOS AND LEONDION) WERE STUDIED. (SHORTENED)","ΔΙΝΕΤΑΙ ΚΑΤ'ΑΡΧΗΝ ΤΟ ΤΕΧΝΙΚΟΓΕΩΛΟΓΙΚΟ ΠΛΑΙΣΙΟ ΤΟΥ ΝΟΜΟΥ ΑΧΑΙΑΣ, ΜΕ ΤΗΝ ΕΚΤΙΜΗΣΗΤΩΝ ΣΥΝΘΗΚΩΝ ΠΟΥ ΔΙΑΜΟΡΦΩΝΟΝΤΑΙ ΚΑΙ ΤΗ ΣΥΝΤΑΞΗ ΤΟΥ ΑΝΤΙΣΤΟΙΧΟΥ ΧΑΡΤΗ ΚΛΙΜΑΚΑΣ 1:100.000, ΣΤΟΝ ΟΠΟΙΟ ΔΙΑΧΩΡΙΖΟΝΤΑΙ 18 ΛΙΘΟΛΟΓΙΚΕΣ ΕΝΟΤΗΤΕΣ. ΣΤΗ ΣΥΝΕΧΕΙΑ, ΔΙΕΡΕΥΝΗΘΗΚΑΝ ΤΑ ΠΛΕΙΟ-ΠΛΕΙΣΤΟΚΑΙΝΙΚΑ ΙΖΗΜΑΤΑ ΚΑΙ ΣΤΙΣ ΤΡΕΙΣ ΛΕΚΑΝΕΣ ΙΖΗΜΑΤΟΓΕΝΕΣΗΣ(ΚΟΡΙΝΘΙΑΚΟΥ, ΠΑΤΡΑΙΚΟΥ ΚΑΙ ΛΕΟΝΤΙΟΥ), ΟΣΟΝ ΑΦΟΡΑ ΣΤΗ ΛΙΘΟΣΤΡΩΜΑΤΟΓΡΑΦΙΚΗ ΤΟΥ ΔΙΑΡΘΡΩΣΗ, ΤΗΝ ΤΕΚΤΟΝΙΚΗ, ΤΗΝ ΟΡΥΚΤΟΛΟΓΙΚΗ ΣΥΣΤΑΣΗ ΚΑΙ ΔΟΜΗ ΚΑΘΩΣ ΚΑΙ ΤΟΥΣ ΦΥΣΙΚΟ- ΜΗΧΑΝΙΚΟΥΣ ΧΑΡΑΚΤΗΡΕΣ. (ΠΕΡΙΚΟΠΗ)"]},{"key":"dc:title","label":"Title","values":["ΤΕΧΝΙΚΟΓΕΩΛΟΓΙΚΕΣ ΣΥΝΘΗΚΕΣ ΣΤΟ ΝΟΜΟ ΑΧΑΙΑΣ-ΓΕΩΜΗΧΑΝΙΚΟΙ ΧΑΡΑΚΤΗΡΕΣ ΤΩΝ ΠΛΕΙΟΠΛΕΙΣΤΟΚΑΙΝΙΚΩΝ ΙΖΗΜΑΤΩΝ","ENGINEERING GEOLOGICAL CONDITIONS IN ACHAIA PROVINCE-GEOMECHANICAL CHARACTERS OF THE PLIOPLEISTOCENE SEDIMENTS"]}]}],"canonical_facts":{"dc:creator":["Ρόζος, Δημήτριος"],"dc:date":["1989"],"dc:description":["THE ENGINEERING-GEOLOGICAL FRAME OF ACHAIA PROVINCE IS GIVEN AT FIRST, BY EVALUATING THE PREDOMINANT CONDITIONS, AND BY DRAWING THE ENGINEERING-GEOLOGICAL MAPOF THE AREA AT A SCALE OF 1:100. 000. IN THIS MAP, 18 LITHOLOGICAL UNITIES AREDISTINGUISHED. FOLLOWING, THE LITHOSTRATIGRAPHY, TECTONICS, MINERALOGICAL COMPOSITION AND FABRIC, AND PHYSICAL AND MECHANICAL PROPERTIES OF THE PLIO-PLEISTOCENE SEDIMENTS FROM THE THREE SEDIMENTATION BASINS (CORINTHIAN, PATRAIKOS AND LEONDION) WERE STUDIED. (SHORTENED)","ΔΙΝΕΤΑΙ ΚΑΤ'ΑΡΧΗΝ ΤΟ ΤΕΧΝΙΚΟΓΕΩΛΟΓΙΚΟ ΠΛΑΙΣΙΟ ΤΟΥ ΝΟΜΟΥ ΑΧΑΙΑΣ, ΜΕ ΤΗΝ ΕΚΤΙΜΗΣΗΤΩΝ ΣΥΝΘΗΚΩΝ ΠΟΥ ΔΙΑΜΟΡΦΩΝΟΝΤΑΙ ΚΑΙ ΤΗ ΣΥΝΤΑΞΗ ΤΟΥ ΑΝΤΙΣΤΟΙΧΟΥ ΧΑΡΤΗ ΚΛΙΜΑΚΑΣ 1:100.000, ΣΤΟΝ ΟΠΟΙΟ ΔΙΑΧΩΡΙΖΟΝΤΑΙ 18 ΛΙΘΟΛΟΓΙΚΕΣ ΕΝΟΤΗΤΕΣ. ΣΤΗ ΣΥΝΕΧΕΙΑ, ΔΙΕΡΕΥΝΗΘΗΚΑΝ ΤΑ ΠΛΕΙΟ-ΠΛΕΙΣΤΟΚΑΙΝΙΚΑ ΙΖΗΜΑΤΑ ΚΑΙ ΣΤΙΣ ΤΡΕΙΣ ΛΕΚΑΝΕΣ ΙΖΗΜΑΤΟΓΕΝΕΣΗΣ(ΚΟΡΙΝΘΙΑΚΟΥ, ΠΑΤΡΑΙΚΟΥ ΚΑΙ ΛΕΟΝΤΙΟΥ), ΟΣΟΝ ΑΦΟΡΑ ΣΤΗ ΛΙΘΟΣΤΡΩΜΑΤΟΓΡΑΦΙΚΗ ΤΟΥ ΔΙΑΡΘΡΩΣΗ, ΤΗΝ ΤΕΚΤΟΝΙΚΗ, ΤΗΝ ΟΡΥΚΤΟΛΟΓΙΚΗ ΣΥΣΤΑΣΗ ΚΑΙ ΔΟΜΗ ΚΑΘΩΣ ΚΑΙ ΤΟΥΣ ΦΥΣΙΚΟ- ΜΗΧΑΝΙΚΟΥΣ ΧΑΡΑΚΤΗΡΕΣ. (ΠΕΡΙΚΟΠΗ)"],"dc:identifier":["10.12681/eadd/1202","http://hdl.handle.net/10442/hedi/1202"],"dc:language":["gre"],"dc:publisher":["University of Patras","Πανεπιστήμιο Πατρών"],"dc:subject":["DIFFERENTIAL THERMAL ANALYSIS (D.T.A.)","ELECTRON SCAN MICROSCOPY","Engineering - geological conditions","GEOMECHANICAL CHARACTERS","GEOTECTONIC STRUCTURES","Physical characteristics","PLIO-PLEISTOCENE SEDIMENTS","SLAKE-DURABILITY","SLOPE MOVEMENTS","X-ray diffraction","ΓΕΩΤΕΚΤΟΝΙΚΕΣ ΔΟΜΕΣ","Διαβρωσιμότητα","ΔΙΑΦΟΡΙΚΗ ΘΕΡΜΙΚΗ ΑΝΑΛΥΣΗ (D.T.A.)","ΗΛΕΚΤΡΟΝΙΚΗ ΜΙΚΡΟΑΝΑΛΥΣΗ","ΚΙΝΗΣΕΙΣ ΠΡΑΝΩΝ","Περιθλασιμετρία ακτίνων - Χ","ΠΛΕΙΟΠΛΕΙΣΤΟΚΑΙΝΙΚΑ ΙΖΗΜΑΤΑ","Τεχνικογεωλογικές συνθήκες","ΦΥΣΙΚΕΣ ΙΔΙΟΤΗΤΕΣ-ΓΕΩΜΗΧΑΝΙΚΟΙ ΧΑΡΑΚΤΗΡΕΣ"],"dc:title":["ΤΕΧΝΙΚΟΓΕΩΛΟΓΙΚΕΣ ΣΥΝΘΗΚΕΣ ΣΤΟ ΝΟΜΟ ΑΧΑΙΑΣ-ΓΕΩΜΗΧΑΝΙΚΟΙ ΧΑΡΑΚΤΗΡΕΣ ΤΩΝ ΠΛΕΙΟΠΛΕΙΣΤΟΚΑΙΝΙΚΩΝ ΙΖΗΜΑΤΩΝ","ENGINEERING GEOLOGICAL CONDITIONS IN ACHAIA PROVINCE-GEOMECHANICAL CHARACTERS OF THE PLIOPLEISTOCENE SEDIMENTS"],"dc:type":["PhD Thesis"]},"updated_at":"2026-07-24T02:24:46Z"}