Structural architecture of the Rhodes Basin: A deep depocentre that evolved since the Pliocene at the junction of Hellenic and Cyprus Arcs, eastern Mediterranean

Keyphrases

• Eastern Mediterranean 100%
• Fault Zone 100%
• Cyprus Arc 100%
• Hellenic Arc 100%
• Structural Architecture 100%
• Miocene 66%
• Fold-and-thrust Belt 66%
• Tectonic Phases 33%
• Transpression 33%
• Late Miocene 33%
• Pliocene-Quaternary 33%
• Subsidence 33%
• Early Pliocene 33%
• Southwestern Turkey 33%
• Lycian Nappes 33%
• Reflector 33%
• Seismic Reflection Profile 33%
• Multichannel Seismic Reflection 33%
• Fethiye-Burdur Fault Zone 33%
• Western Taurides 33%
• Rapid Subsidence 33%
• Strabo 33%
• Messinian 33%
• Sinistral 33%
• Evaporites 33%
• Rhode Island 33%
• Mid-Pliocene 33%
• Transpressional Fault 33%
• Fold-and-thrust 33%
• Pliny 33%
• Regional Subsidence 33%
• Marine Evaporites 33%
• Paleorelief 33%
• Growth Strata 33%
• Obliquity 33%
• African Plate 33%
• Imbricate Thrusts 33%
• Pliny-Strabo Trenches 33%
• Quaternary Phase 33%

Earth and Planetary Sciences

• Pliocene 100%
• Fault Zone 100%
• Depocenter 100%
• Miocene 75%
• Subsidence 75%
• Evaporite 50%
• Trench 25%
• Tectonics 25%
• Transpression 25%
• Seismic Reflection 25%
• Messinian 25%
• African Plate 25%
• Obliquity 25%