1887

Abstract

As aplicaçőes do método gravimétrico em Geocięncias visam basicamente detectar massas anômalas. A representaçăo de anomalias gravimétricas em easis regional é necessária na determinaçăo das ondulasçőes geoidais e das componentes do desvio da vertical, utilizadas no apoio cartográfico em geral e no posicionamento geodésico em particular.

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/content/papers/10.3997/2214-4609-pdb.317.sbgf087
1989-11-20
2020-07-15
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.317.sbgf087
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