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Crustal thickness recovery using an isostatic model and GOCE data
KTH, School of Architecture and the Built Environment (ABE), Urban Planning and Environment, Geodesy and Geoinformatics.
KTH, School of Architecture and the Built Environment (ABE), Urban Planning and Environment, Geodesy and Geoinformatics.
2012 (English)In: Earth Planets and Space, ISSN 1343-8832, E-ISSN 1880-5981, Vol. 64, no 11, 1053-1057 p.Article in journal (Refereed) 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 gradiomet-ric 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.

Place, publisher, year, edition, pages
2012. Vol. 64, no 11, 1053-1057 p.
Keyword [en]
Gradiometry, Isostasy, Moho, Nonlinear ill-posed problem, Tikhonov regularization, continental shelf, crustal thickness, GOCE, gravimetry, satellite mission, Iran
National Category
Geology
Identifiers
URN: urn:nbn:se:kth:diva-129804DOI: 10.5047/eps.2012.04.009ISI: 000312004000007Scopus ID: 2-s2.0-84876387116OAI: oai:DiVA.org:kth-129804DiVA: diva2:654711
Note

QC 20131008

Available from: 2013-10-08 Created: 2013-10-04 Last updated: 2017-12-06Bibliographically approved

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CiteExportLink to record
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Citation style
  • apa
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  • de-DE
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  • nn-NB
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  • Other locale
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Output format
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