[1] In the paper ‘‘Evidence for asymmetric nonvolcanic rifting and slow incipient oceanic accretion from seismic reflection data on the Newfoundland margin’’ by Donna J. Shillington, W. Steven Holbrook, Harm J. A. Van Avendonk, Brian E. Tucholke, John R. Hopper, Keith E. Louden, Hans Christian Larsen, and Gregory T. Nunes (Journal of Geophys ica l Research , 111 , B09402, do i :10 .1029/ 2005JB003981, 2006), the last sentence of section 7 should be changed as follows: [2] Finally, the variable appearance and fault geometries within apparent oceanic basement on the Newfoundland margin suggest extension and an intermittent magma supply during the transition from nonvolcanic rifting to slow incipient oceanic accretion, similar to what is observed on adjacent SCREECH transects [Funck et al., 2003; Hopper et al., 2004; Lau et al., 2006a, 2006b]. JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 111, B12403, doi:10.1029/2006JB004769, 2006 Click Here for Full Article