Dynamic compensation in the central Pacific Ocean [PDF]
The intermediate-wavelength geoid (lambda similar to 2000 km) and sea-floor topography fields in the central Pacific Ocean were studied in terms of static and dynamic compensation models.
Hinojosa, Juan Homero, Marsh, Bruce D.
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Moho Interface Modeling Beneath the Himalayas, Tibet and Central Siberia Using GOCO02S and DTM2006.0
Terrestrial, Atmospheric and Oceanic Sciences, 2013 We apply a newly developed method to estimate the Moho depths and density contrast beneath the Himalayas, Tibet and Central Siberia. This method utilizes the combined least-squares approach based on solving the inverse problem of isostasy and using the ...
Robert Tenzer +3 more
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Impact of GRM: New evidence from the Soviet Union [PDF]
Gravity information released by the Soviet Union allows the quantitative assessment of how the geopotential research mission (GRM) mission might effect the ability to use global gravity data for continental tectonic interpretation.
Mcnutt, M.
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Thermal isostasy on Mars [PDF]
, 2003 Depto. de Geodinámica, Estratigrafía y PaleontologíaFac.
Fairén, Alberto G. +2 more
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Gravity and magnetic anomalies of earthquake-prone areas in the southwestern Ulleung basin margin, East Sea (Sea of Japan). [PDF]
Sci Rep, 2022 Kim CH +5 more
europepmc +1 more source
Viscous relaxation as a probe of heat flux and crustal plateau composition on Venus. [PDF]
Proc Natl Acad Sci U S A, 2023 Nimmo F, Mackwell S.
europepmc +1 more source
Structural Tectonic Scheme Creation Based on Seismic-Gravity Models and Isostasy Usage: Ural Case
Russian Journal of Earth SciencesProcess of Earth’s density models creation leads to the solution of direct and inverse gravimetry problems. The inverse problem of gravimetry is a classic example of an ill-posed problem: in the common statement, its solution is not unique and unstably ...
Martyshko Petr +3 more
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Modeling sea level changes and geodetic variations by glacial isostasy: the improved SELEN code
, 2012 We describe the basic features of SELEN, an open source Fortran 90 program for the numerical solution of the so-called "Sea Level Equation" for a spherical, layered, non-rotating Earth with Maxwell viscoelastic rheology.
Colleoni, Florence +3 more
core
Glacial melting and uplift estimations around the Sør-Rondane Mountains of the East Antarctica since the Pliocene [PDF]
, 2016 第2回極域科学シンポジウム/第31回極域地学シンポジウム 11月16日（水 ...
Miura Hideki +5 more
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