{"id":{"repo_id":"greece","oai_identifier":"oai:10442/1611"},"canonical_url":"https://search.dev.ndltd.org/etd/greece/oai:10442/1611","repository":{"repo_id":"greece","name":"Greek National Archive of PhD Theses","base_url":"https://phdtheses.ekt.gr/eadd_oai/request"},"display":{"title":"Ο ΠΛΟΥΤΩΝΙΤΗΣ ΤΗΣ ΜΑΡΩΝΕΙΑΣ ΚΑΙ Η ΜΕΤΑΜΟΡΦΙΚΗ ΤΟΥ ΕΠΙΔΡΑΣΗ ΣΤΑ ΠΕΡΙΒΑΛΛΟΝΤΑ ΠΕΤΡΩΜΑΤΑ ΤΗΣ ΦΥΛΛΙΤΙΚΗΣ ΣΕΙΡΑΣ","abstract":"THE MARONIA PLUTON HAS A COMPOSITION RANGING FROM MONZODIORITE TO MONZO-GABBRO.THE MONZO-GABBRO COMPOSITION IS DOMINANT. THE PLUTON BELONGS TO THE CALC-ALCALINE ROCK SERIES AND FROM A PETROGENETIC ASPECT IT IS CHARACTERIZED AS AN IGNEOUS ROCK BELONGING TO THE I-TYPE OR MAGNETITE SERIES (M ORIGIN). THE SHALLOW INTRUSION OF THE MARONIA PLUTON DURING ITS CRYSTALLIZATION OF THE MAKRI SERIES WHICH CONSIST OF MARBLES, CALCAREOUS PHYLLITES, GNEISSES, GREENSCHISTS, MICA SCHISTS, AND QUARTZITES. THESE ROCKS HAD UNDERGONE REGIONAL METAMORPHISM BELONGING TOTHE GREENSCHIST FACIES. (SHORTENED)","abstract_html":"THE MARONIA PLUTON HAS A COMPOSITION RANGING FROM MONZODIORITE TO MONZO-GABBRO.THE MONZO-GABBRO COMPOSITION IS DOMINANT. THE PLUTON BELONGS TO THE CALC-ALCALINE ROCK SERIES AND FROM A PETROGENETIC ASPECT IT IS CHARACTERIZED AS AN IGNEOUS ROCK BELONGING TO THE I-TYPE OR MAGNETITE SERIES (M ORIGIN). THE SHALLOW INTRUSION OF THE MARONIA PLUTON DURING ITS CRYSTALLIZATION OF THE MAKRI SERIES WHICH CONSIST OF MARBLES, CALCAREOUS PHYLLITES, GNEISSES, GREENSCHISTS, MICA SCHISTS, AND QUARTZITES. THESE ROCKS HAD UNDERGONE REGIONAL METAMORPHISM BELONGING TOTHE GREENSCHIST FACIES. (SHORTENED)","abstract_has_math":false,"creators":["Δορυφόρου, Αικατερίνη"],"institution":"National Technical University of Athens (NTUA)","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":["CONTACT METAMORPHISM","FLUID INCLUSIONS","FREEZINGTEMPERATURE","GEHLENITE","HOMOGENIZATION TEMPERATURE","HORNFELS","MONZOGABBRO","PETROGRAPHIC TYPE","SKARN","VESURIANITE","ΒΕΖΟΥΒΙΑΝΙΤΗΣ","ΓΚΕΛΕΝΙΤΗΣ","Θερμοκρασία τήξης","ΘΕΡΜΟΚΡΑΣΙΑΟΜΟΓΕΝΟΠΟΙΗΣΗΣ","ΚΕΡΑΤΙΤΗΣ","ΜΕΤΑΜΟΡΦΩΣΗ ΕΠΑΦΗΣ","ΜΕΤΑΣΩΜΑΤΩΣΗ ΕΠΑΦΗΣ","ΜΟΝΖΟΓΑΒΒΡΟΣ","ΠΕΙΡΟΓΡΑΦΙΚΟΣ ΤΥΠΟΣ","ΡΕΥΣΤΑ ΕΓΚΛΕΙΣΜΑΤΑ","Επιστήμες Μηχανικού και Τεχνολογία","Περιβαλλοντική Μηχανική","Engineering and Technology","Environmental Engineering"],"languages":["gre"],"rights":[],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier","label":"Identifier","values":["10.12681/eadd/1611"],"render_values":[{"text":"10.12681/eadd/1611","href":"https://doi.org/10.12681/eadd/1611","code":true}]}]},"links":{"outbound_url":"http://hdl.handle.net/10442/hedi/1611","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:creator","label":"Author","values":["Δορυφόρου, Αικατερίνη"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["1990"]},{"key":"dc:publisher","label":"Institution","values":["National Technical University of Athens (NTUA)","Εθνικό Μετσόβιο Πολυτεχνείο (ΕΜΠ)"]},{"key":"dc:type","label":"Dc Type","values":["PhD Thesis"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["CONTACT METAMORPHISM","FLUID INCLUSIONS","FREEZINGTEMPERATURE","GEHLENITE","HOMOGENIZATION TEMPERATURE","HORNFELS","MONZOGABBRO","PETROGRAPHIC TYPE","SKARN","VESURIANITE","ΒΕΖΟΥΒΙΑΝΙΤΗΣ","ΓΚΕΛΕΝΙΤΗΣ","Θερμοκρασία τήξης","ΘΕΡΜΟΚΡΑΣΙΑΟΜΟΓΕΝΟΠΟΙΗΣΗΣ","ΚΕΡΑΤΙΤΗΣ","ΜΕΤΑΜΟΡΦΩΣΗ ΕΠΑΦΗΣ","ΜΕΤΑΣΩΜΑΤΩΣΗ ΕΠΑΦΗΣ","ΜΟΝΖΟΓΑΒΒΡΟΣ","ΠΕΙΡΟΓΡΑΦΙΚΟΣ ΤΥΠΟΣ","ΡΕΥΣΤΑ ΕΓΚΛΕΙΣΜΑΤΑ","Επιστήμες Μηχανικού και Τεχνολογία","Περιβαλλοντική Μηχανική","Engineering and Technology","Environmental Engineering"]}]},{"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/1611","http://hdl.handle.net/10442/hedi/1611"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["THE MARONIA PLUTON HAS A COMPOSITION RANGING FROM MONZODIORITE TO MONZO-GABBRO.THE MONZO-GABBRO COMPOSITION IS DOMINANT. THE PLUTON BELONGS TO THE CALC-ALCALINE ROCK SERIES AND FROM A PETROGENETIC ASPECT IT IS CHARACTERIZED AS AN IGNEOUS ROCK BELONGING TO THE I-TYPE OR MAGNETITE SERIES (M ORIGIN). THE SHALLOW INTRUSION OF THE MARONIA PLUTON DURING ITS CRYSTALLIZATION OF THE MAKRI SERIES WHICH CONSIST OF MARBLES, CALCAREOUS PHYLLITES, GNEISSES, GREENSCHISTS, MICA SCHISTS, AND QUARTZITES. THESE ROCKS HAD UNDERGONE REGIONAL METAMORPHISM BELONGING TOTHE GREENSCHIST FACIES. (SHORTENED)","Ο ΠΛΟΥΤΩΝΙΤΗΣ ΠΟΥ ΑΠΑΝΤΑΤΑΙ ΣΤΗΝ ΠΕΡΙΟΧΗ ΤΗΣ ΜΑΡΩΝΕΙΑΣ ΕΧΕΙ ΣΥΣΤΑΣΗ ΠΟΥ ΚΥΜΑΙΝΕΤΑΙ ΑΠΟ ΜΟΝΖΟΔΙΟΡΙΤΗ ΕΩΣ ΜΟΝΖΟΓΑΒΒΡΟ ΜΕ ΕΠΙΚΡΑΤΕΣΤΕΡΟ ΤΟΝ ΤΥΠΟ ΤΟΥ ΜΟΝΖΟΓΑΒΒΡΟΥ. ΑΝΗΚΕΙ ΣΤΑ ΑΣΒΕΣΤΑΛΚΑΛΙΚΑ ΠΕΤΡΩΜΑΤΑ ΚΑΙ ΠΕΤΡΟΓΕΝΕΤΙΚΑ ΧΑΡΑΚΤΗΡΙΖΕΤΑΙ ΣΑΝ ΠΥΡΙΓΕΝΕΣ ΠΕΤΡΩΜΑ Ι-ΤΥΠΟΥ 'Η ΣΕΙΡΑΣ ΜΑΓΝΗΤΙΤΗ (ΜΑΓΜΑΤΙΚΗΣ ΠΡΟΕΛΕΥΣΗΣ). Η ΡΗΧΗ ΔΙΕΙΣΔΥΣΗ ΤΟΥ ΠΛΟΥΤΩΝΙΤΗ ΤΗΣ ΜΑΡΩΝΕΙΑΣ ΚΑΤΑ ΤΟ ΣΤΑΔΙΟ ΤΗΣ ΚΡΥΣΤΑΛΛΥΣΗΣ 'Η ΨΥΞΗΣ ΤΟΥ,ΠΡΟΚΑΛΕΣΕ ΦΑΙΝΟΜΕΝΑ ΜΕΤΑΜΟΡΦΩΣΗΣ ΕΠΑΦΗΣ ΣΤΑ ΠΕΤΡΩΜΑΤΑ ΤΗΣ ΕΝΟΤΗΤΑΣ ΜΑΚΡΗΣ ΠΟΥ ΑΠΟΤΕΛΟΥΝΤΑΙ ΑΠΟ ΜΑΡΜΑΡΑ, ΑΣΒΕΣΤΙΤΙΚΟΥΣ ΦΥΛΛΙΤΕΣ, ΓΝΕΥΣΙΟΥΣ ΠΡΑΣΙΝΟΣΧΙΣΤΟΛΙΘΟΥΣ, ΜΑΡΜΑΡΥΓΙΑΚΟΥΣ ΣΧΙΣΤΟΛΙΘΟΥΣ, ΚΑΙ ΧΑΛΑΖΙΤΕΣ. ΤΑ ΠΕΤΡΩΜΑΤΑ ΑΥΤΑ ΕΙΧΑΝ ΥΠΟΣΤΕΙ ΚΑΘΟΛΙΚΗ ΜΕΤΑΜΟΡΦΩΣΗ ΠΡΑΣΙΝΟΣΧΙΣΤΟΛΙΘΙΚΗΣ ΦΑΣΗΣ. (ΠΕΡΙΚΟΠΗ)"]},{"key":"dc:title","label":"Title","values":["Ο ΠΛΟΥΤΩΝΙΤΗΣ ΤΗΣ ΜΑΡΩΝΕΙΑΣ ΚΑΙ Η ΜΕΤΑΜΟΡΦΙΚΗ ΤΟΥ ΕΠΙΔΡΑΣΗ ΣΤΑ ΠΕΡΙΒΑΛΛΟΝΤΑ ΠΕΤΡΩΜΑΤΑ ΤΗΣ ΦΥΛΛΙΤΙΚΗΣ ΣΕΙΡΑΣ","THE MARONIA PLUTON AND ITS METAMORPHIC EFFECTS ON THE SURRONDING ROCKS OF THE PHYLLITE SERIES"]}]}],"canonical_facts":{"dc:creator":["Δορυφόρου, Αικατερίνη"],"dc:date":["1990"],"dc:description":["THE MARONIA PLUTON HAS A COMPOSITION RANGING FROM MONZODIORITE TO MONZO-GABBRO.THE MONZO-GABBRO COMPOSITION IS DOMINANT. THE PLUTON BELONGS TO THE CALC-ALCALINE ROCK SERIES AND FROM A PETROGENETIC ASPECT IT IS CHARACTERIZED AS AN IGNEOUS ROCK BELONGING TO THE I-TYPE OR MAGNETITE SERIES (M ORIGIN). THE SHALLOW INTRUSION OF THE MARONIA PLUTON DURING ITS CRYSTALLIZATION OF THE MAKRI SERIES WHICH CONSIST OF MARBLES, CALCAREOUS PHYLLITES, GNEISSES, GREENSCHISTS, MICA SCHISTS, AND QUARTZITES. THESE ROCKS HAD UNDERGONE REGIONAL METAMORPHISM BELONGING TOTHE GREENSCHIST FACIES. (SHORTENED)","Ο ΠΛΟΥΤΩΝΙΤΗΣ ΠΟΥ ΑΠΑΝΤΑΤΑΙ ΣΤΗΝ ΠΕΡΙΟΧΗ ΤΗΣ ΜΑΡΩΝΕΙΑΣ ΕΧΕΙ ΣΥΣΤΑΣΗ ΠΟΥ ΚΥΜΑΙΝΕΤΑΙ ΑΠΟ ΜΟΝΖΟΔΙΟΡΙΤΗ ΕΩΣ ΜΟΝΖΟΓΑΒΒΡΟ ΜΕ ΕΠΙΚΡΑΤΕΣΤΕΡΟ ΤΟΝ ΤΥΠΟ ΤΟΥ ΜΟΝΖΟΓΑΒΒΡΟΥ. ΑΝΗΚΕΙ ΣΤΑ ΑΣΒΕΣΤΑΛΚΑΛΙΚΑ ΠΕΤΡΩΜΑΤΑ ΚΑΙ ΠΕΤΡΟΓΕΝΕΤΙΚΑ ΧΑΡΑΚΤΗΡΙΖΕΤΑΙ ΣΑΝ ΠΥΡΙΓΕΝΕΣ ΠΕΤΡΩΜΑ Ι-ΤΥΠΟΥ 'Η ΣΕΙΡΑΣ ΜΑΓΝΗΤΙΤΗ (ΜΑΓΜΑΤΙΚΗΣ ΠΡΟΕΛΕΥΣΗΣ). Η ΡΗΧΗ ΔΙΕΙΣΔΥΣΗ ΤΟΥ ΠΛΟΥΤΩΝΙΤΗ ΤΗΣ ΜΑΡΩΝΕΙΑΣ ΚΑΤΑ ΤΟ ΣΤΑΔΙΟ ΤΗΣ ΚΡΥΣΤΑΛΛΥΣΗΣ 'Η ΨΥΞΗΣ ΤΟΥ,ΠΡΟΚΑΛΕΣΕ ΦΑΙΝΟΜΕΝΑ ΜΕΤΑΜΟΡΦΩΣΗΣ ΕΠΑΦΗΣ ΣΤΑ ΠΕΤΡΩΜΑΤΑ ΤΗΣ ΕΝΟΤΗΤΑΣ ΜΑΚΡΗΣ ΠΟΥ ΑΠΟΤΕΛΟΥΝΤΑΙ ΑΠΟ ΜΑΡΜΑΡΑ, ΑΣΒΕΣΤΙΤΙΚΟΥΣ ΦΥΛΛΙΤΕΣ, ΓΝΕΥΣΙΟΥΣ ΠΡΑΣΙΝΟΣΧΙΣΤΟΛΙΘΟΥΣ, ΜΑΡΜΑΡΥΓΙΑΚΟΥΣ ΣΧΙΣΤΟΛΙΘΟΥΣ, ΚΑΙ ΧΑΛΑΖΙΤΕΣ. ΤΑ ΠΕΤΡΩΜΑΤΑ ΑΥΤΑ ΕΙΧΑΝ ΥΠΟΣΤΕΙ ΚΑΘΟΛΙΚΗ ΜΕΤΑΜΟΡΦΩΣΗ ΠΡΑΣΙΝΟΣΧΙΣΤΟΛΙΘΙΚΗΣ ΦΑΣΗΣ. (ΠΕΡΙΚΟΠΗ)"],"dc:identifier":["10.12681/eadd/1611","http://hdl.handle.net/10442/hedi/1611"],"dc:language":["gre"],"dc:publisher":["National Technical University of Athens (NTUA)","Εθνικό Μετσόβιο Πολυτεχνείο (ΕΜΠ)"],"dc:subject":["CONTACT METAMORPHISM","FLUID INCLUSIONS","FREEZINGTEMPERATURE","GEHLENITE","HOMOGENIZATION TEMPERATURE","HORNFELS","MONZOGABBRO","PETROGRAPHIC TYPE","SKARN","VESURIANITE","ΒΕΖΟΥΒΙΑΝΙΤΗΣ","ΓΚΕΛΕΝΙΤΗΣ","Θερμοκρασία τήξης","ΘΕΡΜΟΚΡΑΣΙΑΟΜΟΓΕΝΟΠΟΙΗΣΗΣ","ΚΕΡΑΤΙΤΗΣ","ΜΕΤΑΜΟΡΦΩΣΗ ΕΠΑΦΗΣ","ΜΕΤΑΣΩΜΑΤΩΣΗ ΕΠΑΦΗΣ","ΜΟΝΖΟΓΑΒΒΡΟΣ","ΠΕΙΡΟΓΡΑΦΙΚΟΣ ΤΥΠΟΣ","ΡΕΥΣΤΑ ΕΓΚΛΕΙΣΜΑΤΑ","Επιστήμες Μηχανικού και Τεχνολογία","Περιβαλλοντική Μηχανική","Engineering and Technology","Environmental Engineering"],"dc:title":["Ο ΠΛΟΥΤΩΝΙΤΗΣ ΤΗΣ ΜΑΡΩΝΕΙΑΣ ΚΑΙ Η ΜΕΤΑΜΟΡΦΙΚΗ ΤΟΥ ΕΠΙΔΡΑΣΗ ΣΤΑ ΠΕΡΙΒΑΛΛΟΝΤΑ ΠΕΤΡΩΜΑΤΑ ΤΗΣ ΦΥΛΛΙΤΙΚΗΣ ΣΕΙΡΑΣ","THE MARONIA PLUTON AND ITS METAMORPHIC EFFECTS ON THE SURRONDING ROCKS OF THE PHYLLITE SERIES"],"dc:type":["PhD Thesis"]},"updated_at":"2026-07-24T02:25:02Z"}