{"refrec":{"BRefID":77334,"RR":"<b>Mascle, J.; Chaumillon, E.</b> (1998). An overview of Mediterranean Ridge collisional accretionary complex as deduced from multichannel seismic data. <i>Geo-Mar. Lett. 18(2)</i>: 81-89","BEntID":72939,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Geo-Mar. Lett. 18(2)</i>: 81-89","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Mascle, J.; Chaumillon, E.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Mascle, J.; Chaumillon, E.","Englishabstract":"The Mediterranean Ridge (eastern Mediterranean) is a large accretionary complex that results from the Africa-Europe-Aegean plates convergence. Multichannel seismic data, combined with previous results showed that the ridge comprises distinct major structural domains facing different forelands: (1) An outer domain is bounded to the south by the ridge toe. Underneath the Ionian and Levantine outer Ridge, Messinian evaporites act as a major decollement level. (2) An axial, or crestal, ridge domain with mud diapiric and mud volcano activity is bounded to the north by backthrust. (3) A less tectonized inner Ridge domain, possibly a series of former forearc basins, abuts the Hellenic Trench. The ridge displays strong along-strike variations. 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