Suivre le Chemin du Lapin de Pâques avec un Produit Variant Jusqu'à 100 (A)

In order to test the reliability of electrical tomography and induced polarisation testing as methods for the characterisa- tion of subsurface geological formations and the detection

e. the hangingwall of the fault formed of slickensided dark green garnierite underlying a gently weathered saprolite with a boxwork structure filled by garnierite. It clearly

We compared separately results of Fourier spectrum and HiCum stacking on 365 days data of theoretical tides, grav- ity residuals and barometric pressure (Fig.. The synthetic tides

Finite Element Analysis (FEA) is operated for the first calculation with the initial model parameters to get the input data: optical surface displacements as design responses

Tables 3–5 show the field concentration of trace gases, in- cluding those in equilibrium with aerosol species and their comparison with the modeling results for Finokalia during

More than 2000 kimberlitic eruptions are documented in South Africa on and off the Kaapvaal craton (Figure 1) and some of them brought mantle xenoliths to the Earth’s surface.

measurements for mid-mantle anisotropy in the vicinity of the 660-km discontinuity, the boundary between the upper and lower mantle.. Deep-focus earthquakes in the Tonga±Kermadec

of lithospheric rupture associating ductile transtension of the lithosphere in the early stages of rifting and asthenospheric flow dominantly parallel to the rift