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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Date: | 2016 |
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Main Authors: | , , |
Format: | Article |
Language: | English |
Published: |
Інститут геофізики ім. С.I. Субботіна НАН України
2016
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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. |