(Deniliquin is in the larger brown area) The Deniliquin feature is located beneath the
Murray Sedimentary Basin and partly beneath the
Darling Sedimentary Basin, and centered about northwest of Deniliquin. The principal features of the Deniliquin structure are a multiple ring total magnetic intensity (TMI) pattern with the minimal TMI ring radius of ; a central quiet magnetic zone; circular
Bouguer gravity patterns; an underlying
mantle Moho rise about shallower than under the adjacent
Tasman orogenic zone; and radial faults associated with magnetic and demagnetized anomalies. The above features suggest that the Deniliquin feature is a root zone of a large impact structure, a
multi-ring impact basin. Its existence was proposed by Anthony Yeates somewhere between 1995 and 2000, based upon the magnetic patterns in the area. A 2022 paper by Glikson and Yeates further supports this suggestion based on recent geophysical data, drill-hole samples and airborne magnetic data. , most evidence comes from the surface data. Further confirmation of the suggestion would require further deep drilling. ==Dating==