Gravity 11
Gravity 11 :
The attraction between two masses, such as the Earth and an object on its surface. Commonly referred to as the acceleration of gravity g. Changes in the gravity field can be used to infer information about the structure of the Earth's lithosphere and upper mantle. Interpretations of changes in the gravity field are generally applied to gravity values corrected for extraneous effects. The corrected values are referred to by various terms, such as free-air gravity, Bouguer gravity, and isostatic gravity, depending on the number and kind of corrections made
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