Fig. 3: A comparison of the three-dimensional density model of the Abitibi greenstone belt with previously published Moho depth models.
From: Archean rifts and triple-junctions revealed by gravity modeling of the southern Superior Craton
The map-view of the density model is shown in A and cross-sectional views in B, C. The Moho interface derived from the density model is compared to the Moho derived from the CRUST1.0 global model43, a teleseismic model44, five of the Lithoprobe reflection seismic lines40, and a Lithoprobe seismic refraction model profile41,42, as shown in B, C. In A the Abitibi is outlined in black70.
