The residual gravity map highlights the disposition of high-density shallow source bodies as elliptical highs, located at Narlapur, Kalwakole, and Yelur in the eastern part. These residual gravity ...

Additionally, this survey has indicated numerous unexplored anomalies across the property, further expanding the scope for discovery and emphasizing the strong exploration potential of the area.

This study aims to improve knowledge of the structure of southwest Cameroon based on the analysis and interpretation of gravity data derived from the SGG-UGM-2 model. A residual anomaly map was first ...

New ground gravity data was collected to produce a Bouguer anomaly map and to perform a 3-D inversion in order to obtain a 3-D density model of the central uplift. This 3-D density model is consistent ...

Bouguer gravity anomaly maps show how gravity varies across the Earth’s surface. These maps are created by measuring the pull of gravity at different locations and subtracting the effects of known ...

Figure 1: Gravity data interpretation map showing the 3D gravity targets ... Figure 3: Total bouguer gravity anomaly image and graben fault architecture, overlaying topography.

The absolute gravity values referenced the IGSN-71 (International ... with a maximum amplitude of 6.2 mGal (between -112 and -118.2 mGal) (Figure 5b). Bouguer gravimetric anomaly maps in the main ...

Gravity measurements from the study area were collected as datasets on the deep magmatic structures of the Hawaiian volcanoes. A complete Bouguer anomaly map was constructed from the corrected ...

Residual Bouguer Gravity map of the survey area showing the location of the anomalies relative to the NE-trending syncline of the prospective sulphidic VMS Horizon. The gravity map is overlain on ...

Bathymetry map of the Scotia Sea (SRTM30 Plusv7 ... Figure 3B (inside a white polygon) shows in the north the presence of a gravity gradient zone where Bouguer gravity anomaly values change from low ...