{"id":{"repo_id":"greece","oai_identifier":"oai:10442/1633"},"canonical_url":"https://search.dev.ndltd.org/etd/greece/oai:10442/1633","repository":{"repo_id":"greece","name":"Greek National Archive of PhD Theses","base_url":"https://phdtheses.ekt.gr/eadd_oai/request"},"display":{"title":"ΓΕΩΛΟΓΙΚΕΣ ΚΑΙ ΥΔΡΟΓΕΩΛΟΓΙΚΕΣ ΣΥΝΘΗΚΕΣ ΤΗΣ ΠΕΡΙΟΧΗΣ ΤΟΥ ΤΟΠΟΓΡΑΦΙΚΟΥ ΦΥΛΛΟΥ \"ΜΟΧΟΣ\" (ΚΕΝΤΡΟΑΝΑΤΟΛΙΚΗ ΚΡΗΤΗ)","abstract":"THIS THESIS DEALS WITH THE GEOLOGICAL AND HYDROLOGICAL CONDITIONS OF THE AREA COVERED BY THE TOPOGRAPHIC SHEET \"MOCHOS\" (SCALE 1 : 50,000), AT THE CENTRAL-EASTERN CRETE. THE GEOTECTONIC UNITS CONTRIBUTING TO THE GEOLOGICAL STRUCTURE OF THE STUDY AREA ARE: A) CRETA-MANI UNIT (IDI ZONE OR TALEA ORI GROUP), B) PHYLLITE-QUARTZITE, C) TRIPOLITZA UNIT, D) PINDOS UNIT AND NEOGENE AND QUARTERNARY DEPOSITS. THE STRATIGRAPHY OF THE GEOTECTONIC UNITS HAS BEEN DETERMINED THROUGH SYNTHESIS OF NUMEROUS STRATIGRAPHIC CROSS-SECTIONS; BESIDES THE PALAEOGEOGRAPHIC CONDITIONS OF THE TRIPOLITZA AND PINDOS UNITS HAVE BEEN DESIGNATED AND SPECIAL MENTION IS GIVEN TO NEOGENE DEPOSITS OF PECULIAR COMPOSITIONS WHICH CROP OUT ATHIGH ALTITUDES (UP TO 14OO M). SOME VARISKAN METAMORPHIC ROCKS ARE DESCRIBED; THEY HAVE BEEN FOUND, FOR THE FIRST TIME, INSIDE THE PHYLLITE-QUARTZITE UNIT ATCENTRAL-EASTERN CRETE AND SOME CONCLUSIONS HAS BEEN ARRIVED AT, CONCERNING THENATURE (WHAT IT REPRESENTS) OF THE PQ UNIT, AT THE STUDY AREA AT LEAST.","abstract_html":"THIS THESIS DEALS WITH THE GEOLOGICAL AND HYDROLOGICAL CONDITIONS OF THE AREA COVERED BY THE TOPOGRAPHIC SHEET "MOCHOS" (SCALE 1 : 50,000), AT THE CENTRAL-EASTERN CRETE. THE GEOTECTONIC UNITS CONTRIBUTING TO THE GEOLOGICAL STRUCTURE OF THE STUDY AREA ARE: A) CRETA-MANI UNIT (IDI ZONE OR TALEA ORI GROUP), B) PHYLLITE-QUARTZITE, C) TRIPOLITZA UNIT, D) PINDOS UNIT AND NEOGENE AND QUARTERNARY DEPOSITS. THE STRATIGRAPHY OF THE GEOTECTONIC UNITS HAS BEEN DETERMINED THROUGH SYNTHESIS OF NUMEROUS STRATIGRAPHIC CROSS-SECTIONS; BESIDES THE PALAEOGEOGRAPHIC CONDITIONS OF THE TRIPOLITZA AND PINDOS UNITS HAVE BEEN DESIGNATED AND SPECIAL MENTION IS GIVEN TO NEOGENE DEPOSITS OF PECULIAR COMPOSITIONS WHICH CROP OUT ATHIGH ALTITUDES (UP TO 14OO M). SOME VARISKAN METAMORPHIC ROCKS ARE DESCRIBED; THEY HAVE BEEN FOUND, FOR THE FIRST TIME, INSIDE THE PHYLLITE-QUARTZITE UNIT ATCENTRAL-EASTERN CRETE AND SOME CONCLUSIONS HAS BEEN ARRIVED AT, CONCERNING THENATURE (WHAT IT REPRESENTS) OF THE PQ UNIT, AT THE STUDY AREA AT LEAST.","abstract_has_math":false,"creators":["Αλεξόπουλος, Απόστολος","Alexopoulos, Apostolos"],"institution":"National and Kapodistrian University of Athens","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":"2026-07-24T02:25:02Z","subjects":["ΕΝΟΤΗΤΑ ΚΡΗΤΗΣ-ΜΑΝΗΣ","ΕΝΟΤΗΤΑ ΠΙΝΔΟΥ","ΕΝΟΤΗΤΑ ΤΡΙΠΟΛΗΣ","ΕΝΟΤΗΤΑ ΦΥΛΛΙΤΩΝ-ΧΑΛΑΖΙΤΩΝ","ΚΑΛΥΜΜΑΤΑ","ΚΡΗΤΗ (ΜΟΧΟΣ)","Νεογενές","Παλαιογεωγραφία","Στρωματογραφία","Τεκτονική","Υδρογεωλογία","CRETE (MOCHOS)","CRETE-MANI UNIT (PLATTENKALK)","Hydrogeology","Palaeogeography","PHYLLITE-QUARTZITE","PINDOS UNIT, NEOGENE, NAPPES","Stratigraphy","STRUCTURAL GEOLOGY-NEOTECTONIC","TRIPOLITZA UNIT"],"languages":["gre"],"rights":[],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier","label":"Identifier","values":["10.12681/eadd/1633"],"render_values":[{"text":"10.12681/eadd/1633","href":"https://doi.org/10.12681/eadd/1633","code":true}]}]},"links":{"outbound_url":"http://hdl.handle.net/10442/hedi/1633","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:creator","label":"Author","values":["Αλεξόπουλος, Απόστολος","Alexopoulos, Apostolos"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["1990"]},{"key":"dc:publisher","label":"Institution","values":["National and Kapodistrian University of Athens","Εθνικό και Καποδιστριακό Πανεπιστήμιο Αθηνών (ΕΚΠΑ)"]},{"key":"dc:type","label":"Dc Type","values":["PhD Thesis"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["ΕΝΟΤΗΤΑ ΚΡΗΤΗΣ-ΜΑΝΗΣ","ΕΝΟΤΗΤΑ ΠΙΝΔΟΥ","ΕΝΟΤΗΤΑ ΤΡΙΠΟΛΗΣ","ΕΝΟΤΗΤΑ ΦΥΛΛΙΤΩΝ-ΧΑΛΑΖΙΤΩΝ","ΚΑΛΥΜΜΑΤΑ","ΚΡΗΤΗ (ΜΟΧΟΣ)","Νεογενές","Παλαιογεωγραφία","Στρωματογραφία","Τεκτονική","Υδρογεωλογία","CRETE (MOCHOS)","CRETE-MANI UNIT (PLATTENKALK)","Hydrogeology","Palaeogeography","PHYLLITE-QUARTZITE","PINDOS UNIT, NEOGENE, NAPPES","Stratigraphy","STRUCTURAL GEOLOGY-NEOTECTONIC","TRIPOLITZA UNIT"]}]},{"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/1633","http://hdl.handle.net/10442/hedi/1633"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["THIS THESIS DEALS WITH THE GEOLOGICAL AND HYDROLOGICAL CONDITIONS OF THE AREA COVERED BY THE TOPOGRAPHIC SHEET \"MOCHOS\" (SCALE 1 : 50,000), AT THE CENTRAL-EASTERN CRETE. THE GEOTECTONIC UNITS CONTRIBUTING TO THE GEOLOGICAL STRUCTURE OF THE STUDY AREA ARE: A) CRETA-MANI UNIT (IDI ZONE OR TALEA ORI GROUP), B) PHYLLITE-QUARTZITE, C) TRIPOLITZA UNIT, D) PINDOS UNIT AND NEOGENE AND QUARTERNARY DEPOSITS. THE STRATIGRAPHY OF THE GEOTECTONIC UNITS HAS BEEN DETERMINED THROUGH SYNTHESIS OF NUMEROUS STRATIGRAPHIC CROSS-SECTIONS; BESIDES THE PALAEOGEOGRAPHIC CONDITIONS OF THE TRIPOLITZA AND PINDOS UNITS HAVE BEEN DESIGNATED AND SPECIAL MENTION IS GIVEN TO NEOGENE DEPOSITS OF PECULIAR COMPOSITIONS WHICH CROP OUT ATHIGH ALTITUDES (UP TO 14OO M). SOME VARISKAN METAMORPHIC ROCKS ARE DESCRIBED; THEY HAVE BEEN FOUND, FOR THE FIRST TIME, INSIDE THE PHYLLITE-QUARTZITE UNIT ATCENTRAL-EASTERN CRETE AND SOME CONCLUSIONS HAS BEEN ARRIVED AT, CONCERNING THENATURE (WHAT IT REPRESENTS) OF THE PQ UNIT, AT THE STUDY AREA AT LEAST.","ΣΤΗ ΔΙΑΤΡΙΒΗ ΑΥΤΗ ΔΙΕΡΕΥΝΟΝΤΑΙ ΟΙ ΓΕΩΛΟΓΙΚΕΣ ΚΑΙ ΥΔΡΟΓΕΩΛΟΓΙΚΕΣ ΣΥΝΘΗΚΕΣ ΤΗΣ ΠΕΡΙΟΧΗΣ ΠΟΥ ΚΑΛΥΠΤΕΤΑΙ ΑΠΟ ΤΟ ΤΟΠΟΓΡΑΦΙΚΟ ΦΥΛΛΟ \"ΜΟΧΟΣ\", ΚΛΙΜΑΚΑΣ 1 : 50.000, ΣΤΗΝ ΚΕΝΤΡΟΑΝΑΤΟΛΙΚΗ ΚΡΗΤΗ. ΣΤΗΝ ΓΕΩΛΟΓΙΚΗ ΔΟΜΗ ΤΗΣ ΠΕΡΙΟΧΗΣ ΣΥΜΜΕΤΕΧΟΥΝ ΟΙ ΓΕΩΤΕΚΤΟΝΙΚΕΣ ΕΝΟΤΗΤΕΣ ΚΡΗΤΗΣ-ΜΑΝΗΣ, ΦΥΛΛΙΤΩΝ-ΧΑΛΑΖΙΤΩΝ, ΤΡΙΠΟΛΗΣ, ΠΙΝΔΟΥ, ΚΑΘΩΣ ΚΑΙΑΠΟΘΕΣΕΙΣ ΤΟΥ ΝΕΟΓΕΝΟΥΣ ΚΑΙ ΤΟΥ ΤΕΤΑΡΤΟΓΕΝΟΥΣ. ΜΕ ΤΗ ΣΥΝΘΕΣΗ ΠΟΛΥΑΡΙΘΜΩΝ ΣΤΡΩΜΑΤΟΓΡΑΦΙΚΩΝ ΤΟΜΩΝ ΚΑΘΟΡΙΖΕΤΑΙ Η ΣΤΡΩΜΑΤΟΓΡΑΦΙΑ ΤΩΝ ΔΙΑΦΟΡΩΝ ΓΕΩΤΕΚΤΟΝΙΚΩΝ ΕΝΟΤΗΤΩΝ, ΚΑΘΟΡΙΖΟΝΤΑΙ ΟΙ ΠΑΛΑΙΟΓΕΩΓΡΑΦΙΚΕΣ ΣΥΝΘΗΚΕΣ ΤΩΝ ΕΝΟΤΗΤΩΝ ΤΡΙΠΟΛΗΣ ΚΑΙ ΠΙΝΔΟΥ ΚΑΙ ΓΙΝΕΤΑΙ ΙΔΙΑΙΤΕΡΗ ΜΝΕΙΑ ΣΕ ΙΔΙΟΡΡΥΘΜΗΣ ΣΥΣΤΑΣΗΣ ΝΕΟΓΕΝΕΙΣ ΑΠΟΘΕΣΕΙΣ ΠΟΥ ΑΠΑΝΤΟΥΝ ΣΕ ΜΕΓΑΛΑ ΥΨΟΜΕΤΡΑ (ΜΕΧΡΙ 14ΟΟΜ). ΠΕΡΙΓΡΑΦΟΝΤΑΙ ΒΑΡΙΣΚΙΑ ΜΕΤΑΜΟΡΦΩΜΕΝΑ ΠΕΤΡΩΜΑΤΑ ΠΟΥ ΓΙΑ ΠΡΩΤΗ ΦΟΡΑ ΕΝΤΟΠΙΣΤΗΚΑΝ ΕΝΤΟΣ ΤΩΝ ΦΥΛΛΙΤΩΝ-ΧΑΛΑΖΙΤΩΝ ΣΤΗΝ ΚΕΝΤΡΟΑΝΑΤΟΛΙΚΗ ΚΡΗΤΗ ΚΑΙ ΕΞΑΓΟΝΤΑΙ ΣΥΜΠΕΡΑΣΜΑΤΑ ΣΧΕΤΙΚΑ ΜΕ ΤΟ ΤΙ ΑΝΤΙΠΡΟΣΩΠΕΥΕΙ ΗΕΝΟΤΗΤΑ ΦΥΛΛΙΤΩΝ-ΧΑΛΑΖΙΤΩΝ ΤΟΥΛΑΧΙΣΤΟΝ ΓΙΑ ΤΗΝ ΠΕΡΙΟΧΗ ΜΕΛΕΤΗΣ. (ΠΕΡΙΚΟΠΗ)"]},{"key":"dc:title","label":"Title","values":["ΓΕΩΛΟΓΙΚΕΣ ΚΑΙ ΥΔΡΟΓΕΩΛΟΓΙΚΕΣ ΣΥΝΘΗΚΕΣ ΤΗΣ ΠΕΡΙΟΧΗΣ ΤΟΥ ΤΟΠΟΓΡΑΦΙΚΟΥ ΦΥΛΛΟΥ \"ΜΟΧΟΣ\" (ΚΕΝΤΡΟΑΝΑΤΟΛΙΚΗ ΚΡΗΤΗ)","GEOLOGICAL AND HYDROGEOLOGICAL CONDITIONS AT THE AREA OF \"MOCHOS\" TOPOGRAPHIC SHEET (CENTRAL-WESTERN CRETE)"]}]}],"canonical_facts":{"dc:creator":["Αλεξόπουλος, Απόστολος","Alexopoulos, Apostolos"],"dc:date":["1990"],"dc:description":["THIS THESIS DEALS WITH THE GEOLOGICAL AND HYDROLOGICAL CONDITIONS OF THE AREA COVERED BY THE TOPOGRAPHIC SHEET \"MOCHOS\" (SCALE 1 : 50,000), AT THE CENTRAL-EASTERN CRETE. THE GEOTECTONIC UNITS CONTRIBUTING TO THE GEOLOGICAL STRUCTURE OF THE STUDY AREA ARE: A) CRETA-MANI UNIT (IDI ZONE OR TALEA ORI GROUP), B) PHYLLITE-QUARTZITE, C) TRIPOLITZA UNIT, D) PINDOS UNIT AND NEOGENE AND QUARTERNARY DEPOSITS. THE STRATIGRAPHY OF THE GEOTECTONIC UNITS HAS BEEN DETERMINED THROUGH SYNTHESIS OF NUMEROUS STRATIGRAPHIC CROSS-SECTIONS; BESIDES THE PALAEOGEOGRAPHIC CONDITIONS OF THE TRIPOLITZA AND PINDOS UNITS HAVE BEEN DESIGNATED AND SPECIAL MENTION IS GIVEN TO NEOGENE DEPOSITS OF PECULIAR COMPOSITIONS WHICH CROP OUT ATHIGH ALTITUDES (UP TO 14OO M). SOME VARISKAN METAMORPHIC ROCKS ARE DESCRIBED; THEY HAVE BEEN FOUND, FOR THE FIRST TIME, INSIDE THE PHYLLITE-QUARTZITE UNIT ATCENTRAL-EASTERN CRETE AND SOME CONCLUSIONS HAS BEEN ARRIVED AT, CONCERNING THENATURE (WHAT IT REPRESENTS) OF THE PQ UNIT, AT THE STUDY AREA AT LEAST.","ΣΤΗ ΔΙΑΤΡΙΒΗ ΑΥΤΗ ΔΙΕΡΕΥΝΟΝΤΑΙ ΟΙ ΓΕΩΛΟΓΙΚΕΣ ΚΑΙ ΥΔΡΟΓΕΩΛΟΓΙΚΕΣ ΣΥΝΘΗΚΕΣ ΤΗΣ ΠΕΡΙΟΧΗΣ ΠΟΥ ΚΑΛΥΠΤΕΤΑΙ ΑΠΟ ΤΟ ΤΟΠΟΓΡΑΦΙΚΟ ΦΥΛΛΟ \"ΜΟΧΟΣ\", ΚΛΙΜΑΚΑΣ 1 : 50.000, ΣΤΗΝ ΚΕΝΤΡΟΑΝΑΤΟΛΙΚΗ ΚΡΗΤΗ. ΣΤΗΝ ΓΕΩΛΟΓΙΚΗ ΔΟΜΗ ΤΗΣ ΠΕΡΙΟΧΗΣ ΣΥΜΜΕΤΕΧΟΥΝ ΟΙ ΓΕΩΤΕΚΤΟΝΙΚΕΣ ΕΝΟΤΗΤΕΣ ΚΡΗΤΗΣ-ΜΑΝΗΣ, ΦΥΛΛΙΤΩΝ-ΧΑΛΑΖΙΤΩΝ, ΤΡΙΠΟΛΗΣ, ΠΙΝΔΟΥ, ΚΑΘΩΣ ΚΑΙΑΠΟΘΕΣΕΙΣ ΤΟΥ ΝΕΟΓΕΝΟΥΣ ΚΑΙ ΤΟΥ ΤΕΤΑΡΤΟΓΕΝΟΥΣ. ΜΕ ΤΗ ΣΥΝΘΕΣΗ ΠΟΛΥΑΡΙΘΜΩΝ ΣΤΡΩΜΑΤΟΓΡΑΦΙΚΩΝ ΤΟΜΩΝ ΚΑΘΟΡΙΖΕΤΑΙ Η ΣΤΡΩΜΑΤΟΓΡΑΦΙΑ ΤΩΝ ΔΙΑΦΟΡΩΝ ΓΕΩΤΕΚΤΟΝΙΚΩΝ ΕΝΟΤΗΤΩΝ, ΚΑΘΟΡΙΖΟΝΤΑΙ ΟΙ ΠΑΛΑΙΟΓΕΩΓΡΑΦΙΚΕΣ ΣΥΝΘΗΚΕΣ ΤΩΝ ΕΝΟΤΗΤΩΝ ΤΡΙΠΟΛΗΣ ΚΑΙ ΠΙΝΔΟΥ ΚΑΙ ΓΙΝΕΤΑΙ ΙΔΙΑΙΤΕΡΗ ΜΝΕΙΑ ΣΕ ΙΔΙΟΡΡΥΘΜΗΣ ΣΥΣΤΑΣΗΣ ΝΕΟΓΕΝΕΙΣ ΑΠΟΘΕΣΕΙΣ ΠΟΥ ΑΠΑΝΤΟΥΝ ΣΕ ΜΕΓΑΛΑ ΥΨΟΜΕΤΡΑ (ΜΕΧΡΙ 14ΟΟΜ). ΠΕΡΙΓΡΑΦΟΝΤΑΙ ΒΑΡΙΣΚΙΑ ΜΕΤΑΜΟΡΦΩΜΕΝΑ ΠΕΤΡΩΜΑΤΑ ΠΟΥ ΓΙΑ ΠΡΩΤΗ ΦΟΡΑ ΕΝΤΟΠΙΣΤΗΚΑΝ ΕΝΤΟΣ ΤΩΝ ΦΥΛΛΙΤΩΝ-ΧΑΛΑΖΙΤΩΝ ΣΤΗΝ ΚΕΝΤΡΟΑΝΑΤΟΛΙΚΗ ΚΡΗΤΗ ΚΑΙ ΕΞΑΓΟΝΤΑΙ ΣΥΜΠΕΡΑΣΜΑΤΑ ΣΧΕΤΙΚΑ ΜΕ ΤΟ ΤΙ ΑΝΤΙΠΡΟΣΩΠΕΥΕΙ ΗΕΝΟΤΗΤΑ ΦΥΛΛΙΤΩΝ-ΧΑΛΑΖΙΤΩΝ ΤΟΥΛΑΧΙΣΤΟΝ ΓΙΑ ΤΗΝ ΠΕΡΙΟΧΗ ΜΕΛΕΤΗΣ. (ΠΕΡΙΚΟΠΗ)"],"dc:identifier":["10.12681/eadd/1633","http://hdl.handle.net/10442/hedi/1633"],"dc:language":["gre"],"dc:publisher":["National and Kapodistrian University of Athens","Εθνικό και Καποδιστριακό Πανεπιστήμιο Αθηνών (ΕΚΠΑ)"],"dc:subject":["ΕΝΟΤΗΤΑ ΚΡΗΤΗΣ-ΜΑΝΗΣ","ΕΝΟΤΗΤΑ ΠΙΝΔΟΥ","ΕΝΟΤΗΤΑ ΤΡΙΠΟΛΗΣ","ΕΝΟΤΗΤΑ ΦΥΛΛΙΤΩΝ-ΧΑΛΑΖΙΤΩΝ","ΚΑΛΥΜΜΑΤΑ","ΚΡΗΤΗ (ΜΟΧΟΣ)","Νεογενές","Παλαιογεωγραφία","Στρωματογραφία","Τεκτονική","Υδρογεωλογία","CRETE (MOCHOS)","CRETE-MANI UNIT (PLATTENKALK)","Hydrogeology","Palaeogeography","PHYLLITE-QUARTZITE","PINDOS UNIT, NEOGENE, NAPPES","Stratigraphy","STRUCTURAL GEOLOGY-NEOTECTONIC","TRIPOLITZA UNIT"],"dc:title":["ΓΕΩΛΟΓΙΚΕΣ ΚΑΙ ΥΔΡΟΓΕΩΛΟΓΙΚΕΣ ΣΥΝΘΗΚΕΣ ΤΗΣ ΠΕΡΙΟΧΗΣ ΤΟΥ ΤΟΠΟΓΡΑΦΙΚΟΥ ΦΥΛΛΟΥ \"ΜΟΧΟΣ\" (ΚΕΝΤΡΟΑΝΑΤΟΛΙΚΗ ΚΡΗΤΗ)","GEOLOGICAL AND HYDROGEOLOGICAL CONDITIONS AT THE AREA OF \"MOCHOS\" TOPOGRAPHIC SHEET (CENTRAL-WESTERN CRETE)"],"dc:type":["PhD Thesis"]},"updated_at":"2026-07-24T02:25:02Z"}