Free-air gravity anomalies for Egypt. Contour interval: 10 mgal

Traditional Airy-Heiskanen isostatic anomalies for Egypt. Contour

Geological Examples of the Flexure Model of Isostasy (Chapter 4) - Isostasy and Flexure of the Lithosphere

Novel technique for the interpretation of gravity anomalies over geologic structures with idealized geometries using the Manta ray foraging optimization - ScienceDirect

Hussein ABD-ELMOTAAL, Professor of Surveying & Geodesy, Former Head of Department, B.Sc., M.Sc., Ph.D., Minia University, Al Minyā, Department of Civil Engineering

Sensitivity of DIN and OP to a change of constituent loadings.

Correlation coefficients between different residual data of geoids.

Toward 1-mGal accuracy in global marine gravity from CryoSat-2, Envisat, and Jason-1

Sensitivity of DIN and OP to a change of constituent loadings.

Sensitivity of DIN and OP to a change of constituent loadings.

Differences of GPS Levelling geoid and extended GRACE/GOCE model

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