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- W2567070810 abstract "espanolRecientes trabajos de campo nos permiten llegar a una nueva lectura del conjunto de datos asi como a la nueva interpretacion que resulta de los mismos Distinguimos por ende, para el conjunto de las Hellenidas, cinco unidades paleo-geograficas mayores, escalonadas entre Paleo Africa y Europa, quienes, mediantes fases tectonicas superpuestas - y no paralelas, ni tampoco de igual desplazamiento, conformaron el edifico actual: • Una plataforma carbonatada arabo-africana, incluyendo variaciones laterales y longitudinales. • Una zona de transicion entre la plataforma carbonatada y las ofiolitas tethysianas. • Una zona de ‘’mezcla colorada’’ tectonica • Las ofiolitas tethysianas, material mantelico de tipo oceanico. • La masa continental herciniana . EnglishThis study is based on some new field observations made on the group of the Eastern Hellenic regions. Our observations have led us to adopt a simplified view of the paleogeography of the Greek mainland before the Alpine orogenesis. The subsequent varied tectonic units originate mainly from the following paleogeographic areas: • A carbonate Arabo-African shelf margin which displays several lateral transitions, ridges and basins. On the Greek mainland this margin is represented by the Preapulian, Ionian, Gavrovo-Tripolis, Parnassos zones, the Olympus platform and probably the Kavala and Thassos marble. • A transition zone from the shelf units to the Tethys ophiolites (Pindos Zone, Styra, Argolis and Hydra, Eretrias new unit). • Tethys ophiolites, which might represent either an “ocean” fault zone or subduction of the lithosphere along a weak area. • A Hercynian continental mass (Serbomacedonian). This group is currently completed by the presence of a large tectonic melange connected to the ophiolite overthrust." @default.
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- W2567070810 date "2016-01-01" @default.
- W2567070810 modified "2023-09-24" @default.
- W2567070810 title "Structure and history of Hellenides" @default.
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