Fig. 8From: Application of the normalized largest eigenvalue of structure tensor in the interpretation of potential field tensor dataGravity anomaly caused by salt dome near Houston (Nettleton 1976) and the calculated tensor component. a Bouguer gravity anomaly; b gravity gradient component \({f}_{zx}\); c gravity gradient component \({f}_{zy}\). The white line in Fig. 8a is the cross section for Fig. 9Back to article page