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Paleomagnetic and rock magnetic data from sedimentary core collected at high ...
This dataset includes paleomagnetic and rock magnetic analyses from four sediment cores collected on continental slope of Storfjorden (EG-02, EG-03, SV-04) and Kveithola... -
Solutions of ocean tide loading displacement, self-attraction and loading and...
As a supplement to Huang et al. (2022) “The influence of sediments, lithosphere and upper mantle (anelastic) with lateral heterogeneity on ocean tide loading and ocean tide... -
3D thermal model of the southern Central Andes
The Central Andean orogen formed as a result of the subduction of the oceanic Nazca plate beneath the continental South-American plate. In the southern segment of the Central... -
Experimental data for permeability and stiffness measurements of fractured Fl...
Faults and fractures form the largest contrast of fluid flow in the subsurface, while their permeability is highly affected by effective pressure changes. In this experimental... -
Stress strain data of experimentally deformed Carrara marble in the semi-brit...
The data set contains stress-strain data of Carrara marble experimentally deformed in triaxial compression at temperatures of 20 – 800°C, confining pressures of 30 – 300 MPa,... -
Creep data of (Dotternhausen) Posidonia shale
Experimentally determined data to examine the creep behavior of an immature carbonate-rich Posidonia shale (Dottenhausen), subjected to constant stress conditions at... -
Lithospheric-scale 3D model of the Southern Central Andes
The Central Andean orogeny is caused by the subduction of the Nazca oceanic plate beneath the South-American continental plate. In Particular, the Southern Central Andes (SCA,... -
3D Gravity Constrained Model of Density Distribution Across the Alpine Lithos...
The Alps are one of the best studied mountain ranges in the world, yet significant unknowns remain regarding their crustal structure and density distribution at depth. Previous...
