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

Characteristics of gravity anomalies and tectonic analysis of Enderby Land in East Antarctica and its adjacent areas

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

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Physics of The Earth, PDF, Geophysics

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

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

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

Location of the GPS/BM stations used in the test campaign (T campaign).

Full article: Comparative analysis of the structural pattern over the Indian Ocean basins using EIGEN6C4 Bouguer gravity data

Correlation coefficients between different residual data of geoids.

PREPARATION OF THE FREE-AIR GRAVITY ANOMALY MAP IN THE LAND AND SEAS OF CHINA AND ADJACENT AREAS USING MULTI-SOURCE GRAVITY DATA AND INTERPRETATION OF THE GRAVITY FIELD

Regional gravity anomaly map (Contour Interval 0.3 mGal), and (b

Map : Bouguer gravity maps (1 milligal contour interval) of the Dyson, Shoals Junction and Abbeville East quadrangles. Maps and gravity station data

KGS--Bulletin 237--Geophysical Model from Potential-field Data in

On the use of gravity data in delineating geologic features of interest for geothermal exploration in the Geneva Basin (Switzerland): prospects and limitations, Swiss Journal of Geosciences

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