Gongola Basin Geoid Determination using Isostatic Models and Seismic Reflection Data and Geophysical Interpretation

The application of Stokes’ formula to create geoid undulation requires no masses outside the geoid. Usually, a constant density of 2.67g / cm3 is used in the determination of the geoid which introduces error in the reduced gravity anomalies (Helmert’s condensation) and consequently the geoid. In th...

Full description

Bibliographic Details

Main Authors:	E.E. Epuh, J.B. Olaleye, O.G. Omogunloye
Format:	Artigo
Language:	Inglês
Published:	Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine 2016-12-01
Series:	Геофизический журнал
Subjects:	geoid undulation Airy-Heiskanen model Pratt-Hayford model isostatic residual gravity anomaly residual geoid undulation
Online Access:	https://journals.uran.ua/geofizicheskiy/article/view/91883
Tags:	Add Tag No Tags, Be the first to tag this record!