In this study, we present a new method to compute the gravity field and gravity gradient
tensor caused by tesseroid mass bodies in the spherical coordinate system. Using this new …

Temporal variations in the Earth's gravity field can be used for monitoring of lithospheric
deformations. The network of continuously operating gravity stations is required for this …

Sub-lithospheric stresses can be estimated by analysis of gravity field measurements.
Depending on the measured gravimetric quantity, different methods can be employed to …

The sublithospheric stress due to mantle convection can be computed from gravity data and
propagated through the lithosphere by solving the boundary-value problem of elasticity for …

Two integral transformations between the stress function, differentiation of which gives the
meridian and prime vertical components of the sub-crustal stress due to mantle convection …

The exploitation of GOCE gradiometer data for validation and interpretation purposes in
local and regional scales requires specific pre-processing steps. The released gradiometer …

Mass changes and flow in the Earth's mantle causes the Earth's crust not only to move
vertically, but also horizontally and to tilt, and produce a major stress in the lithosphere. Here …

National report of Sweden to the NKG General Assembly 2018 Page 1 DAN NORINa, ANNA
BO JENSENb, MOHAMMAD BAGHERBANDIc, MEHDI ESHAGHd NATIONAL REPORT …