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
doaj +1 more source
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
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
core +1 more source
The Thermal and Rheological Structures of the Lithosphere of Tibetan Plateau [PDF]
, 2013 HKT-ISTP 2013 ...
Wang, Yang
core
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
doaj +1 more source
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
Erosion as a driving mechanism of intracontinental mountain growth [PDF]
, 1996 In nature, mountains can grow and remain as localized tectonic features over long periods of time (> 10 m.y.). By contrast, according to current knowledge of lithospheric rheology and neglecting surface processes, any intracontinental range with a width ...
Avouac, J. P., Burov, E. B.
core
Geoid Anomalies and the Near-Surface Dipole Distribution of Mass [PDF]
Although geoid or surface gravity anomalies cannot be uniquely related to an interior distribution of mass, they can be related to a surface mass distribution.
Ockendon, J. R., Turcotte, D. L.
core +1 more source
Upward and outward growth of north-central Tibet: Mechanisms that build high-elevation, low-relief plateaus. [PDF]
Sci Adv, 2023 Li L, Garzione CN.
europepmc +1 more source