ΓΕΩΛΟΓΙΚΗ ΔΟΜΗ ΚΑΙ ΓΕΩΔΥΝΑΜΙΚΗ ΕΞΕΛΙΞΗ ΤΗΣ ΟΡΟΣΕΙΡΑΣ ΤΟΥ ΚΟΖΙΑΚΑ (ΔΥΤΙΚΗ ΘΕΣΣΑΛΙΑ)

THE OBJECT OF EXAMINATION IS THE GEOLOGICAL STRUCTURE OF THE KOZAKAS RANGE, WHICH IS CONSTRUCTED MAINLY BY FORMATIONS OF THE WESTERN THESSALY UNIT, AGED UPPERTRIASSIC-MIDDLE-UPPER EOCENE. AFTER STUDIES ON THE LITHOSTRATIGRAPHY TECTONIC,STRUCTURE AND DEFORMATION, THERE HAS BEEN CONFIRMED THAT DURING THE IURASSIC PERIOD WAS THE MAIN AREAS OF SEDIMENTATION WERE A) A PLATFORM WITH HERITIC SEDIMENTATION B) A SLOPE BY THE PLATFORM WITH PELAGIC- ABYSIAL SEDIMENTS AND OPHIOLITES. THE REPRESENTATION OF THE PALAEOGEOGRAPHY OF THE UNIT'S REGION LED TO ITS POSITIONING IN THE TETHYS SYSTEM.

Grantor dc:publisher

National and Kapodistrian University of Athens

Year dc:date

1988

Authors dc:creator

• Λέκκας, Ευθύμιος
• Lekkas, Efthymios

• Γεωδυναμική εξέλιξη
• Γεωλογική δομή
• Ελλάδα
• Θεσσαλία
• Κόζιακας
• ΛΙΘΟΣΤΡΩΜΑΤΟΓΡΑΦΙΚΗ ΔΙΑΡΘΡΩΣΗ
• Οφιόλιθοι
• ΤΕΚΤΟΝΙΚΗ ΔΟΜΗ-ΠΑΡΑΜΟΡΦΩΣΗ
• ΩΚΕΑΝΟΣ ΔΥΤΙΚΗΣ ΘΕΣΣΑΛΙΑΣ
• Geodynamic evolution
• Geological structure
• Hellas
• Koziakas
• LITHOSTRATIGRAPHY STRUCTURE
• OFIOLITE
• TECTONIC STRUCTURE
• Thessaly
• WEST THESSALY BASIN

Language dc:language

gre

Identifier

10.12681/eadd/0634

OAI identifier oai:identifier

oai:10442/0634