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Buchanan

書目名稱Gravity Interpretation影響因子(影響力)




書目名稱Gravity Interpretation影響因子(影響力)學科排名




書目名稱Gravity Interpretation網絡公開度




書目名稱Gravity Interpretation網絡公開度學科排名




書目名稱Gravity Interpretation被引頻次




書目名稱Gravity Interpretation被引頻次學科排名




書目名稱Gravity Interpretation年度引用




書目名稱Gravity Interpretation年度引用學科排名




書目名稱Gravity Interpretation讀者反饋




書目名稱Gravity Interpretation讀者反饋學科排名

陳腐的人

fleeting

Infant

municipality

Observations and Field Activities,ements with gravimeters for the purpose of deriving gravity anomalies and interpreting them in geological terms. Anomalies are characteristic gravity variations which are to be defined or constructed from ensembles of observations at point sets, usually at the Earth’s surface, and they are related t

未完成

Gravity Anomalies and Disturbances: Reductions and Analyses, latter are usually obscured by the other influences which must be removed in order to reveal the geological information. This cleaning operation is called “.” and the results are called anomalies of various kinds which are the target of interpretation. Proper reductions require knowledge of the sta

未完成

Qualitative Interpretation,ht” or also “of the right order”, while “quantitative” means “numerically correct”. “Principally right” implies that an interpretation envisages the right type of model; “of the right order” denotes a different aspect, namely “semi-quantitative” or “approximate” with low requirements on accuracy, ef

Palate

Quantitative Interpretation,s. There is no clear distinction between “qualitative” and “quantitative”. “Quantitative” is never “absolutely accurate” or error-free, and model parameters must be complemented by their error bounds. What is considered sufficiently accurate depends on the study aims, data situation, numerical reali

antecedence

The Travails of Democratization in Liberia,tion of the Earth are governed by the central force of gravity counteracted mainly by the molecular and atomic forces against compression and deformation. Ongoing geodynamic processes are driven mainly by thermal disturbances of the equilibrium which gravity tries to achieve, to maintain or to resto

Obstacle

Ivan Potravnyi,Ulrich Wei?enburgerth’s gravitation and the rotational or centrifugal acceleration. Its value is roughly 9.81±0.03?m/s. at the Earth’s surface. A small part is time-varying. Gravity decreases with distance from the surface, both upward (Newton’s law) and from some depth also downward (as only the masses below the obse