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 2.67 g/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 this...

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Bibliographic Details
Date:2016
Main Authors: Epuh, E.E., Olaleye, J.B., Omogunloye, O.G.
Format: Article
Language:English
Published: Інститут геофізики ім. С.I. Субботіна НАН України 2016
Series:Геофизический журнал
Online Access:http://dspace.nbuv.gov.ua/handle/123456789/125227
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Journal Title:Digital Library of Periodicals of National Academy of Sciences of Ukraine
Cite this:Gongola Basin Geoid Determination using Isostatic Models and Seismic Reflection Data and Geophysical Interpretation / E.E. Epuh, J.B. Olaleye, O.G. Omogunloye // Геофизический журнал. — 2016. — Т. 38, № 6. — С. 137-151. — Бібліогр.: 74 назв. — англ.

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Digital Library of Periodicals of National Academy of Sciences of Ukraine