Mud diapirs are present in different tectonic environments around the globe and are particularly prevalent in large deltas. The onshore, Jurassic-Cretaceous Recvo Basin NE Brazil, represents an atypical example of mud diapir occurrence in a rift basin. The intensity of mud diapirism is different in the three sectors of the basin, with the central sector exhibiting the best development In the southern sector, diapirism is less significant, and it is practically non-existent in the northeast sector. 3D seismic, outcrop and well data were used to geomorphologically characterize the onshore mud diapirs in the central sector of the Recvo Basin and correlate them with the structural and morphological aspects of the basin, in addition to elucidating the possible origins of their movement. After seismic interpretation, four mud diapirs were identified in the study area: Apraius-Miranga Norte, Pedra do Salgado, Biriba and Carijwo internal seismic facies were identified as F1 and F2, with F1 presenting more disruptive features and F2 being more reflection-free. The eastern diapirs, close to border fault conglomerates, are dominated by disrupted seismic facies (F1). The diapiric movement is associated with paleo-seismicity and the rupture of an ancient delta front together with rapid basinward advancement of conglomerates during an active rifting phase. The Biriba diapir was possibly the first to arise, followed by Carijpraius-Miranga Norte and lastly Pedra do Salgado; this variable timing influenced the location and migration of depocenters in the area. #xD;Keywords: Mud diapir; Recvo Basin; 3D seismic interpretation. #xD;