A crustal thickness model of Antarctica calculated in spherical approximation from satellite gravimetric data

Author:

Chisenga Chikondi12,Yan Jianguo13,Yan Peng4

Affiliation:

1. State Key Laboratory of Information Engineering in Surveying, Mapping and Remote Sensing, Wuhan University, Box 129, Luoyu Road, Wuhan 430079, China

2. Department of Earth Sciences, Ndata School of Climate and Earth Sciences, Malawi University of Science and Technology, P.O. Box 5196, Limbe, Malawi

3. Instituto de Astronomia y Ciencias Planetarias de Atacama, Universidad de Atacama, Copayapu 485, Chile

4. Chinese Antarctic Center of Surveying and Mapping, Wuhan University, Box 129, Luoyu Road, Wuhan 430079, China

Funder

National Key Research and Development Project

National Scientific Foundation of China

Innovation Group of Natural Fund of Hubei

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Reference72 articles.

1. Moho-depth and subglacial sedimentary layer thickness in the Wilkes Basin from receiver function analysis;Agostinetti,2005

2. On the computation of the effect of the attraction of mountain-masses, as disturbing the apparent astronomical latitude of stations in geodetic surveys;Airy;Phil. Trans. R. Soc. Lond. A,1855

3. S-velocity model and inferred Moho topography beneath the Antarctic Plate from Rayleigh waves;An;J. geophys. Res.,2015

4. The DNSC08GRA global marine gravity field from double retracked satellite altimetry;Andersen;J. Geod.,2010

5. The Moho depth map of the Antarctica region;Baranov;Tectonophysics,2013

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