Fig. 6From: High-resolution gravity and geoid models in Tahiti obtained from new airborne and land gravity observations: data fusion by spectral combinationFree-air gravity anomaly models of Tahiti. The two models (see Table 7) are from: a EGM08 to degree 1500, airborne and altimeter gravity (1500+a+o). b All datasets (1500+a+o+t+l). The topographic contours are shown at a 500-m intervalBack to article page