{"refrec":{"BRefID":77615,"RR":"<b>Mougenot, D.; Hernandez, J.; Virlogeux, P.</b> (1989). Structure et volcanisme d'un rift sous-marin: Le fossé des Kérimbas (marge nord - Mozambique). <i>Bull. Soc. Géol. Fr. 5(2)</i>: 401-410","BEntID":73171,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Bull. Soc. Géol. Fr. 5(2)</i>: 401-410","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Mougenot, D.; Hernandez, J.; Virlogeux, P.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Mougenot, D. <i>et al.</i>","Englishabstract":"On the continental margin of the northern Mozambique, a flat-bottomed trough, the north-south trending Kerimbas deep graben, disrupts the continental slope alongside an alignment of seamounts forming the Davie Ridge. Water-gun seismic reflection lines, implemented throughout the region during MD40/MACAMO cruise, show that the graben, cut into Tertiary sediments, corresponds : eastward, to a former discontinuity several times reactivated and located above an abrupt uplift of the Moho; westward, to a Miocene tilting or a recent normal fault. On both sides and at its southern end, the graben supports alkaline basalts intrusive into Neogene sediments. 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