Due to the complexity and overlap effects of gravity anomalies, the gravity high point always deviates from the real position of the target. Researching the offset characteristics is helpful to determine the right location of gravity anomalies. In this paper, a series of forward models were designed to calculate the offset features under different assumptions. Different density models were established based on the measured gravity data in north China Sunhu area and a variety of methods were tried to eliminate offset effects under different conditions. The results indicate that the gravity anomalies of different density bodies can be separated effectively and the real position of target can be correctly located by using the “layer stripping method”.
HESS - Evaluating downscaling methods of GRACE (Gravity Recovery and Climate Experiment) data: a case study over a fractured crystalline aquifer in southern India
Frontiers Structural architecture and late Cenozoic tectonic evolution of the Ulsan Fault Zone, SE Korea: New insights from integration of geological and geophysical data
The gravity high point offset in different density of the buried hill A.
A vertical cross-section through a 3D density model from the
Information about the coastal gravity surveys in three offshore areas
Towards a high-resolution time-variable gravity field model for sub-regional scale investigations
Geophysical Modeling with Satellite Gravity Data: Eigen-6C4 vs. GGM Plus
Black-hole masses as a function of horizon radius r 0 , with a crossing
Witten diagram for a three-point function.
3D inversion of full gravity gradient tensor data in spherical coordinate system using local north-oriented frame, Earth, Planets and Space
A vertical cross-section through a 3D density model from the
The original and processed gravity responses of model III.
Different forms of the AdS/CFT correspondence
Experimental profile of a 2D gravity current
