Together with Iceland, the two giant oceanic plateaux, Ontong Java in
the western Pacific and Kerguelen/Broken Ridge in the Indian Ocean, ar
e accumulations of mafic igneous rock which were not formed by 'normal
' seafloor spreading. We compare published geochronological, crustal s
tructure, and subsidence results with tectonic fabric highlighted in n
ew satellite-derived free-air gravity data from the three igneous prov
inces, and conclude that existing evidence weighs lightly against the
Ontong Java and Kerguelen plateaux originating at a seafloor spreading
centre.