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Improved global crustal thickness modeling based on the VMM isostatic model and non-isostatic gravity correction

Bagherbandi, Mohammad (author)
Högskolan i Gävle,KTH,Geodesi och geoinformatik,Samhällsbyggnad/GIS-Institutet,Geodesy
Tenzer, Robert (author)
Wuhan University, China
Sjöberg, Lars E. (author)
KTH,Geodesi och geoinformatik,Royal Institute of Technology (KTH), Stockholm, Sweden
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Novak, Pavel (author)
University of West Bohemia, Plzen, Czech Republic
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 (creator_code:org_t)
Elsevier BV, 2013
2013
English.
In: Journal of Geodynamics. - : Elsevier BV. - 0264-3707 .- 1879-1670. ; 66, s. 25-37
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • In classical isostatic models for a gravimetric recovery of the Moho parameters (i.e., Moho depths and density contrast) the isostatic gravity anomalies are usually defined based on the assumption that the topographic mass surplus and the ocean mass deficiency are compensated within the Earth's crust. As acquired in this study, this assumption yields large disagreements between isostatic and seismic Moho models. To assess the effects not accounted for in classical isostatic models, we conduct a number of numerical experiments using available global gravity and crustal structure models. First, we compute the gravitational contributions of mass density contrasts due to ice and sediments, and subsequently evaluate respective changes in the Moho geometry. Residual differences between the gravimetric and seismic Moho models are then used to predict a remaining non-isostatic gravity signal, which is mainly attributed to unmodeled density structures and other geophysical phenomena. We utilize three recently developed computational schemes in our numerical studies. The apparatus of spherical harmonic analysis and synthesis is applied in forward modeling of the isostatic gravity disturbances. The Moho depths are estimated globally on a 1 arc-deg equiangular grid by solving the Vening-Meinesz Moritz inverse problem of isostasy. The same estimation model is applied to evaluate the differences between the isostatic and seismic models. We demonstrate that the application of the ice and sediment density contrasts stripping gravity corrections is essential for a more accurate determination of the Moho geometry. We also show that the application of the additional non-isostatic correction further improves the agreement between the Moho models derived based on gravity and seismic data. Our conclusions are based on comparing the gravimetric results with the CRUST2.0 global crustal model compiled using results of seismic surveys.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geofysik (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geophysics (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Annan geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Other Earth and Related Environmental Sciences (hsv//eng)

Keyword

Earth's crust
Gravity
Isostasy
Mantle
Mass density
Moho interface

Publication and Content Type

ref (subject category)
art (subject category)

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