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Crustal thickness recovery using an isostatic model and GOCE data
Royal Institute of Technology (KTH),Division of Geodesy and Geoinformatics .
Royal Institute of Technology (KTH),Division of Geodesy and Geoinformatics, .ORCID-id: 0000-0003-0067-8631
2012 (engelsk)Inngår i: Earth Planets and Space, ISSN 1343-8832, E-ISSN 1880-5981, Vol. 64, nr 11, s. 1053-1057Artikkel i tidsskrift, Letter (Fagfellevurdert) Published
Abstract [en]

One of the GOCE satellite mission goals is to study the Earth's interior structure including its crustal thickness. A gravimetric-isostatic Moho model, based on the Vening Meinesz-Moritz (VMM) theory and GOCE gradiometric data, is determined beneath Iran's continental shelf and surrounding seas. The terrestrial gravimetric data of Iran are also used in a nonlinear inversion for a recovering-Moho model applying the VMM model. The newly-computed Moho models are compared with the Moho data taken from CRUST2.0. The root-mean-square (RMS) of differences between the CRUST2.0 Moho model and the recovered model from GOCE and that from the terrestrial gravimetric data are 3.8 km and 4.6 km, respectively.

sted, utgiver, år, opplag, sider
2012. Vol. 64, nr 11, s. 1053-1057
Emneord [en]
Isostasy, Tikhonov regularization, Moho, nonlinear ill-posed problem, gradiometry
HSV kategori
Forskningsprogram
TEKNIK
Identifikatorer
URN: urn:nbn:se:hv:diva-5304DOI: 10.5047/eps.2012.04.009ISI: 000312004000007OAI: oai:DiVA.org:hv-5304DiVA, id: diva2:617367
Tilgjengelig fra: 2013-04-23 Laget: 2013-04-23 Sist oppdatert: 2017-12-06bibliografisk kontrollert

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