A gravimetric method to determine horizontal stress field due to flow in the mantle in Fennoscandia

Author:

Gido Nureldin Ahmed Adam,Bagherbandi Mohammad,Sjöberg Lars E.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences,General Environmental Science

Reference67 articles.

1. Bagherbandi, M. 2011, An isostatic Earth crustal model and its applications. Doctoral Dissertation in Geodesy, Royal Institute of Technology (KTH), Division of Geodesy, and Geoinformatics, Stockholm, 240 p.

2. Bagherbandi, M. and Sjöberg L.E. 2012, Non-isostatic effects on crustal thickness: A study using CRUST2.0 in Fennoscandia. Physics of the Earth and Planetary Interiors, 200–201, 37–44.

3. Bagherbandi, M. and Sjöberg, L.E. 2013, Improving gravimetric-isostatic models of crustal depth by correcting for non-isostatic effects and using CRUST2.0. Earth Science Review, 117, 29–39.

4. Bai, W., Vigny, C., Ricard, Y., and Froidevaux, C. 1992, On the origin of deviatoric stresses in the lithosphere. Journal of Geophysical Research, 97, 11,729–11,737.

5. Boulton, G.S. and Payn, A. 1993, Simulation of the European ice sheet through the last glacial cycle and prediction of future glaciation. Swedish Nuclear Fuels and Waste Management Company, Progress Report 14–93, Stockholm, 138 p.

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