A newly distinguished marine magnetotelluric coast effect sensitive to the lithosphere–asthenosphere boundary [PDF]
Shunguo Wang +3 more
openalex +1 more source
Melting for the generation of intracontinental diffuse basaltic fields is generally ascribed to the effects from lithospheric dynamic processes, but how the asthenospheric dynamics influence the overlying lithosphere remains poorly known.
Hong‐Kun Dai +2 more
doaj +1 more source
A multilayer model of time dependent deformation following an earthquake on a strike-slip fault [PDF]
A multilayer model of the Earth to calculate finite element of time dependent deformation and stress following an earthquake on a strike slip fault is discussed. The model involves shear properties of an elastic upper lithosphere, a standard viscoelastic
Cohen, S. C.
core +1 more source
Delamination Magmatism in Eastern Anatolia: A Geochemical Perspective
The Sr‐Nd‐Hf‐Pb isotope geochemistry of the Late Miocene Tunceli Volcanics suggests that they are the products of mixed asthenospheric and lithospheric mantle melts.
Alican Aktağ +3 more
doaj +1 more source
Satellite magnetic modeling of north African hot spots [PDF]
The primary objectives of the MAGSAT mission was to measure the intensity and direction of magnetization of the Earth's crust. A significant effort was directed to the large crustal anomalies first delineated by the POGO mission.
Brown, C. R., Phillips, R. J.
core +1 more source
Resolving the lithosphere-asthenosphere boundary with seismic Rayleigh waves [PDF]
Stefan Bartzsch +2 more
openalex +1 more source
Lithospheric Structure Above the Northern Appalachian Anomaly: Initial Results From the NEST Array
Seismic tomography observations show a low‐velocity feature in the upper mantle beneath eastern North America known as the Northern Appalachian Anomaly (NAA).
Kimberly Espinal +3 more
doaj +1 more source
Postseismic viscoelastic surface deformation and stress. Part 1: Theoretical considerations, displacement and strain calculations [PDF]
A model of viscoelastic deformations associated with earthquakes is presented. A strike-slip fault is represented by a rectangular dislocation in a viscoelastic layer (lithosphere) lying over a viscoelastic half-space (asthenosphere).
Cohen, S. C.
core +1 more source
Heterogeneous rheology controlled postseismic deformation of the 2011 Tohoku‐Oki earthquake
Using two‐dimensional finite element modeling, we reproduced the observed postseismic deformation of the 2011 Tohoku‐Oki earthquake. Our model, which accounts for the lithosphere‐asthenosphere boundary and weak zones beneath volcanoes, was able to ...
Jun Muto +6 more
doaj +1 more source

