Gravity data distribution and Bouguer gravity anomaly map of the study

Download scientific diagram | Gravity data distribution and Bouguer gravity anomaly map of the study area (Contour interval: 5 mGals; color-scale unit: mGal; projection: Mercator). Data are recorded at stations shown here as black cross and were collected following all available roads and tracks. from publication: 3D Mafic Topography of the Transition Zone between the North-Western Boundary of the Congo Craton and the Kribi-Campo Sedimentary Basin from Gravity Inversion | The structure of the transition zone between the north-western boundary of the Congo Craton and the Kribi-Campo sedimentary basin is still a matter of scientific debate. In this study, the existing gravity data are interpreted in order to better understand the geodynamics of | Congo, Sedimentary Basins and Topography | ResearchGate, the professional network for scientists.

Use of the Polynomial Separation and the Gravity Spectral Analysis to Estimate the Depth of the Northern Logone Birni Sedimentary Basin (CAMEROON)

International Journal of Geophysics

Grid map expanded using the Maximum Entropy Method (Burg, 1967)

Distribution of gravity data and Bouguer anomaly map of the study area.

Bouguer Anomaly - an overview

Regression analysis between gravity and equivalent topography: a)

Philippe Njandjock Nouck's research works University of Yaoundé II, Yaoundé and other places

a Bouguer gravity anomaly map generated from 345 gravity station

3D Mafic Topography of the Transition Zone between the North-Western Boundary of the Congo Craton and the Kribi-Campo Sedimentary Basin from Gravity Inversion - Document - Gale Academic OneFile

Mouzong MARCELIN, Doctor of Engineering, University of Buea, Buea, Renewable Energy, Higher Technical Teachers' Training College

DS 411: Michigan Magnetic and Gravity Maps and Data: A Website for the Distribution of Data

PDF) 3D Mafic Topography of the Transition Zone between the North-Western Boundary of the Congo Craton and the Kribi-Campo Sedimentary Basin from Gravity Inversion