Fig. 3From: High-resolution gravity and geoid models in Tahiti obtained from new airborne and land gravity observations: data fusion by spectral combinationResults of the Tahiti airborne gravity survey after the crossover adjustment. a Free-air gravity anomalies at the flight altitude. b Gravity differences at crossover points. The numbers near the lines are the flight numbers. The triangle shows the location of the TAHI base stationBack to article page