{"id":{"repo_id":"greece","oai_identifier":"oai:10442/0185"},"canonical_url":"https://search.dev.ndltd.org/etd/greece/oai:10442/0185","repository":{"repo_id":"greece","name":"Greek National Archive of PhD Theses","base_url":"https://phdtheses.ekt.gr/eadd_oai/request"},"display":{"title":"ΜΕΤΑΛΛΟΓΕΝΕΣΗ ΤΗΣ ΤΡΙΤΟΓΕΝΟΥΣ ΘΕΙΟΥΧΟΥ ΜΕΤΑΛΛΟΦΟΡΙΑΣ ΠΕΡΙΟΧΗΣ ΑΙΣΥΜΗΣ ΝΟΜΟΥ ΕΒΡΟΥ","abstract":"THE ESSIMI AREA IS PART OF THE ESSIMI-KIRKI TERTIARY BASIN. IT IS MADE UP FROMSEDIMENTARY AND VOLCANIC ROCKS. THE SEDIMENTARY SEQUENCE CONSISTS OF ALTERNATIONS OF ARENACEOUS AND ARGILLACEOUS ROCKS, WHEREAS THE IGNEOUS ROCKS COMPRISE SUBVOLCANIC INTRUSIVES, LAVAS AND PYROCLASTICS. THE VOLCANIC ROCKS ARE ANDESITES AND DACITES OF ANDEAN- TYPE CALC-ALCALINE AFFINITY, FORMED IN INTRACONTINENTAL RIFT-BASINS. (SHORTENED)","abstract_html":"THE ESSIMI AREA IS PART OF THE ESSIMI-KIRKI TERTIARY BASIN. IT IS MADE UP FROMSEDIMENTARY AND VOLCANIC ROCKS. THE SEDIMENTARY SEQUENCE CONSISTS OF ALTERNATIONS OF ARENACEOUS AND ARGILLACEOUS ROCKS, WHEREAS THE IGNEOUS ROCKS COMPRISE SUBVOLCANIC INTRUSIVES, LAVAS AND PYROCLASTICS. THE VOLCANIC ROCKS ARE ANDESITES AND DACITES OF ANDEAN- TYPE CALC-ALCALINE AFFINITY, FORMED IN INTRACONTINENTAL RIFT-BASINS. (SHORTENED)","abstract_has_math":false,"creators":["Katirtzoglou, Konstantinos","Κατιρτζόγλου, Κωνσταντίνος"],"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":1986,"date_issued":"1986","date_published":"1986","updated_at":"2026-07-24T02:25:08Z","subjects":["Γεωλογία","Ζώνωση","Μεταλλογένεση","ΟΙΚΟΝΟΜΙΚΗ ΓΕΩΛΟΓΙΑ","EMIGRATION DEPOSITION SEA WATER","HYDROTHERMAL METALLIFERONS FLUIDS","METALLOGENESIS","ZANATION"],"languages":["gre"],"rights":[],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier","label":"Identifier","values":["10.12681/eadd/0185"],"render_values":[{"text":"10.12681/eadd/0185","href":"https://doi.org/10.12681/eadd/0185","code":true}]}]},"links":{"outbound_url":"http://hdl.handle.net/10442/hedi/0185","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:creator","label":"Author","values":["Katirtzoglou, Konstantinos","Κατιρτζόγλου, Κωνσταντίνος"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["1986"]},{"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":["Γεωλογία","Ζώνωση","Μεταλλογένεση","ΟΙΚΟΝΟΜΙΚΗ ΓΕΩΛΟΓΙΑ","EMIGRATION DEPOSITION SEA WATER","HYDROTHERMAL METALLIFERONS FLUIDS","METALLOGENESIS","ZANATION"]}]},{"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/0185","http://hdl.handle.net/10442/hedi/0185"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["THE ESSIMI AREA IS PART OF THE ESSIMI-KIRKI TERTIARY BASIN. IT IS MADE UP FROMSEDIMENTARY AND VOLCANIC ROCKS. THE SEDIMENTARY SEQUENCE CONSISTS OF ALTERNATIONS OF ARENACEOUS AND ARGILLACEOUS ROCKS, WHEREAS THE IGNEOUS ROCKS COMPRISE SUBVOLCANIC INTRUSIVES, LAVAS AND PYROCLASTICS. THE VOLCANIC ROCKS ARE ANDESITES AND DACITES OF ANDEAN- TYPE CALC-ALCALINE AFFINITY, FORMED IN INTRACONTINENTAL RIFT-BASINS. (SHORTENED)","Η ΠΕΡΙΟΧΗ ΑΙΣΥΜΗΣ ΑΠΟΤΕΛΕΙ ΤΜΗΜΑ ΤΗΣ ΤΡΙΤΟΓΕΝΟΥΣ ΛΕΚΑΝΗΣ ΑΙΣΥΜΗΣ- ΚΙΡΚΗΣ ΚΑΙ ΔΟΜΕΙΤΑΙ ΑΠΟ ΙΖΗΜΑΤΟΓΕΝΕΙΣ ΚΑΙ ΗΦΑΙΣΤΕΙΟΓΕΝΕΙΣ ΣΧΗΜΑΤΙΣΜΟΥΣ. ΤΑ ΙΖΗΜΑΤΟΓΕΝΗ ΠΕΤΡΩΜΑΤΑ ΣΥΝΙΣΤΟΥΝ ΟΙ ΨΑΜΜΙΤΟΠΗΛΙΤΙΚΕΣ ΕΝΑΛΛΑΓΕΣ ΤΑ ΔΕ ΗΦΑΙΣΤΕΙΟΓΕΝΗ, ΤΑ ΔΙΕΙΣΔΥΤΙΚΑ ΣΩΜΑΤΑ ΜΕ ΤΙΣ ΠΑΡΑΓΩΓΕΣ ΜΟΡΦΕΣ ΤΟΥΣ, ΟΙ ΛΑΒΕΣ ΚΑΙ ΤΑ ΠΥΡΟΚΛΑΣΤΙΚΑ. ΤΑ ΗΦΑΙΣΤΕΙΟΓΕΝΗ ΠΕΤΡΩΜΑΤΑ ΕΧΟΥΝ ΑΣΒΕΣΤΑΛΚΑΛΙΚΟ ΧΑΡΑΚΤΗΡΑ, ΤΑΞΙΝΟΜΟΥΝΤΑΙ ΣΕ ΑΝΔΕΣΙΤΕΣΚΑΙ ΔΑΚΙΤΕΣ, ΑΝΗΚΟΥΝ ΣΕ ΟΡΟΓΕΝΕΤΙΚΕΣ ΣΕΙΡΕΣ ΤΟΥ ΤΥΠΟΥ ΤΩΝ ΑΝΔΕΩΝ ΚΑΙ ΣΧΗΜΑΤΙΣΘΗΚΑΝ ΣΕ ΕΝΔΟ-ΗΠΕΙΡΩΤΙΚΕΣ ΛΕΚΑΝΕΣ ΠΟΥ ΣΥΝΔΕΟΝΤΑΙ ΜΕ ΦΑΙΝΟΜΕΝΑ ΕΦΕΛΚΥΣΜΟΥ. (ΠΕΡΙΚΟΠΗ)"]},{"key":"dc:title","label":"Title","values":["ΜΕΤΑΛΛΟΓΕΝΕΣΗ ΤΗΣ ΤΡΙΤΟΓΕΝΟΥΣ ΘΕΙΟΥΧΟΥ ΜΕΤΑΛΛΟΦΟΡΙΑΣ ΠΕΡΙΟΧΗΣ ΑΙΣΥΜΗΣ ΝΟΜΟΥ ΕΒΡΟΥ","THE METALLOGENESIS OF THE TERTIARY SULPHIDE MINERALIZATION OF THE ESSIMI REGION, EVROS COUNTY"]}]}],"canonical_facts":{"dc:creator":["Katirtzoglou, Konstantinos","Κατιρτζόγλου, Κωνσταντίνος"],"dc:date":["1986"],"dc:description":["THE ESSIMI AREA IS PART OF THE ESSIMI-KIRKI TERTIARY BASIN. IT IS MADE UP FROMSEDIMENTARY AND VOLCANIC ROCKS. THE SEDIMENTARY SEQUENCE CONSISTS OF ALTERNATIONS OF ARENACEOUS AND ARGILLACEOUS ROCKS, WHEREAS THE IGNEOUS ROCKS COMPRISE SUBVOLCANIC INTRUSIVES, LAVAS AND PYROCLASTICS. THE VOLCANIC ROCKS ARE ANDESITES AND DACITES OF ANDEAN- TYPE CALC-ALCALINE AFFINITY, FORMED IN INTRACONTINENTAL RIFT-BASINS. (SHORTENED)","Η ΠΕΡΙΟΧΗ ΑΙΣΥΜΗΣ ΑΠΟΤΕΛΕΙ ΤΜΗΜΑ ΤΗΣ ΤΡΙΤΟΓΕΝΟΥΣ ΛΕΚΑΝΗΣ ΑΙΣΥΜΗΣ- ΚΙΡΚΗΣ ΚΑΙ ΔΟΜΕΙΤΑΙ ΑΠΟ ΙΖΗΜΑΤΟΓΕΝΕΙΣ ΚΑΙ ΗΦΑΙΣΤΕΙΟΓΕΝΕΙΣ ΣΧΗΜΑΤΙΣΜΟΥΣ. ΤΑ ΙΖΗΜΑΤΟΓΕΝΗ ΠΕΤΡΩΜΑΤΑ ΣΥΝΙΣΤΟΥΝ ΟΙ ΨΑΜΜΙΤΟΠΗΛΙΤΙΚΕΣ ΕΝΑΛΛΑΓΕΣ ΤΑ ΔΕ ΗΦΑΙΣΤΕΙΟΓΕΝΗ, ΤΑ ΔΙΕΙΣΔΥΤΙΚΑ ΣΩΜΑΤΑ ΜΕ ΤΙΣ ΠΑΡΑΓΩΓΕΣ ΜΟΡΦΕΣ ΤΟΥΣ, ΟΙ ΛΑΒΕΣ ΚΑΙ ΤΑ ΠΥΡΟΚΛΑΣΤΙΚΑ. ΤΑ ΗΦΑΙΣΤΕΙΟΓΕΝΗ ΠΕΤΡΩΜΑΤΑ ΕΧΟΥΝ ΑΣΒΕΣΤΑΛΚΑΛΙΚΟ ΧΑΡΑΚΤΗΡΑ, ΤΑΞΙΝΟΜΟΥΝΤΑΙ ΣΕ ΑΝΔΕΣΙΤΕΣΚΑΙ ΔΑΚΙΤΕΣ, ΑΝΗΚΟΥΝ ΣΕ ΟΡΟΓΕΝΕΤΙΚΕΣ ΣΕΙΡΕΣ ΤΟΥ ΤΥΠΟΥ ΤΩΝ ΑΝΔΕΩΝ ΚΑΙ ΣΧΗΜΑΤΙΣΘΗΚΑΝ ΣΕ ΕΝΔΟ-ΗΠΕΙΡΩΤΙΚΕΣ ΛΕΚΑΝΕΣ ΠΟΥ ΣΥΝΔΕΟΝΤΑΙ ΜΕ ΦΑΙΝΟΜΕΝΑ ΕΦΕΛΚΥΣΜΟΥ. (ΠΕΡΙΚΟΠΗ)"],"dc:identifier":["10.12681/eadd/0185","http://hdl.handle.net/10442/hedi/0185"],"dc:language":["gre"],"dc:publisher":["National and Kapodistrian University of Athens","Εθνικό και Καποδιστριακό Πανεπιστήμιο Αθηνών (ΕΚΠΑ)"],"dc:subject":["Γεωλογία","Ζώνωση","Μεταλλογένεση","ΟΙΚΟΝΟΜΙΚΗ ΓΕΩΛΟΓΙΑ","EMIGRATION DEPOSITION SEA WATER","HYDROTHERMAL METALLIFERONS FLUIDS","METALLOGENESIS","ZANATION"],"dc:title":["ΜΕΤΑΛΛΟΓΕΝΕΣΗ ΤΗΣ ΤΡΙΤΟΓΕΝΟΥΣ ΘΕΙΟΥΧΟΥ ΜΕΤΑΛΛΟΦΟΡΙΑΣ ΠΕΡΙΟΧΗΣ ΑΙΣΥΜΗΣ ΝΟΜΟΥ ΕΒΡΟΥ","THE METALLOGENESIS OF THE TERTIARY SULPHIDE MINERALIZATION OF THE ESSIMI REGION, EVROS COUNTY"],"dc:type":["PhD Thesis"]},"updated_at":"2026-07-24T02:25:08Z"}