From Satellite Gradiometry Data to Subcrustal Stress Due to Mantle Convection

Author:

Eshagh Mehdi

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference48 articles.

1. Bagherbandi M. (2011) An isostatic Earth crustal model and its application, Doctoral Dissertation in Geodesy, Royal Institute of Technology (KTH), Stockholm, Sweden.

2. Bagherbandi M. and Eshagh M. (2011) Recovery of Moho’s undulations based on the Vening Meinesz–Moritz theory from satellite gravity gradiometry data: A simulation study, Adv. Space Res., 49(6):1097–1111.

3. Bagherbandi M. and Eshagh M. (2012) Crustal thickness recovery using an isostatic model and GOCE data, EPS, 64(11):1053–1057.

4. Bassin C., Laske G., and Masters G. (2000) The current limits of resolution for surface wave tomography in North America, EOS trans AGU, 81, F897.

5. Bruinsma S.L., Marty J.C., Balmino G., Biancale R., Foerste C., Abrikosov O. and Neumayer H. (2010) GOCE Gravity Field Recovery by Means of the Direct Numerical Method, presented at the ESA Living Planet Symposium, 27th June–2nd July 2010, Bergen, Norway; see also: earth.esa.int/GOCE.

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