The exploitation of state of the art digital terrain databases and combined or satellite-only Earth gravity models for the estimation of the crust–mantle interface over oceanic regions

Author:

Arabelos D.N.,Tsoulis D.

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Reference19 articles.

1. Global marine gravity field from the ERS-1 and Geosat geodetic mission altimetry;Andersen;J. geophys. Res.,1998

2. Moho depths in the Indian Ocean based on the inversion of satellite gravity data;Arabelos,2006

3. The collocation approach to the inversion of gravity dada;Barzaghi;Geophys. Prospect.,1992

4. The currrent limits of resolution for surface wave tomography in North America;Bassin,2000

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1. Processing aspects of level 2 GOCE gradiometer data for regional applications;Geophysical Journal International;2018-11-16

2. Local Recovery of Sub-Crustal Stress Due to Mantle Convection from Satellite-to-Satellite Tracking Data;Acta Geophysica;2016-08

3. Complete gravity field of an ellipsoidal prism by Gauss–Legendre quadrature;Geophysical Journal International;2015-11-05

4. GOCE data, models, and applications: A review;International Journal of Applied Earth Observation and Geoinformation;2015-03

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