Abstract
Models of convergence between the major African and European plates involve a stretching Aegean plate, whose present motion relative to Africa is south-west1–3. This motion has resulted in subduction of eastern Mediterranean sea floor as shown by seismicity, volcanism and morphology. The southern boundary of the Aegean plate is formed by the Hellenic Trench. Intensive study, culminating in the use of submersibles and multibeam echo-sounding as part of the Hellenic Arc and Trench Program4, has outlined the complexity of this boundary. Detailed reflection profiling which we carried out in autumn 1980 of the eastern portion of the Hellenic Trench system shows arcward verging thrusting south-west of the Rhodes Basin. We conclude that collision of the African continental margin with the Hellenic Arc is now in progress, causing overriding by the Mediterranean Ridge along the southeastern branch of the Hellenic Trench system.
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Jongsma, D., Mascle, J. Evidence for northward thrusting south-west of the Rhodes Basin. Nature 293, 49–51 (1981). https://doi.org/10.1038/293049a0
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DOI: https://doi.org/10.1038/293049a0
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