… From the database of the Eifel plume project with nearly 200 recorded teleseismic events …
, body wave magnitude larger than 4.9 and a clearly correlated wavefront of a S-wave phase (S …

… sional (P) and shear (S) waves and the analysis of the P-coda … from surface wave dispersion
studies, teleseismic shear-wave … 2% for compressional waves and 5% for shear waves in its …

… We obtain well-resolved 1-D models of the shear wave velocity v s under the Eifel region,
Central Europe, from teleseismic surface waves. Using 41 temporary and permanent broad-…

… Eifel is depressed by 15–25 km, which could be explained by a maximum temperature increase
of +200C to +300C. In the 3-D RF image of the Eifel Plume … upper mantle plume but they …

… plume models are able to explain the P-wave traveltime anomalies observed during the Eifel
plume … the plume location, temperature anomaly, plume flux and relative motion between …

… To image the mantle structure of the proposed Eifel plume with high resolution to a depth of
at least 400 km, 10 European institutions operated a seismic network with an aperture of 500…

… We then examine models of SWS at the Eifel, Hawaiian, and Iceland … shear wave splitting
reflects a greater amount shear between the plate and plume on the upwind side of the plume …

… from a smaller total heat flux plume trapped beneath a thicker … Eifel Plume would be small
compared to the degree of decompression melting of the higher heat flux Icelandic Plume …

… shear-wave splitting analysis across the Eifel hotspot in west-central Europe. Our data set
includes 18 permanent European broadband stations and 102 temporary Eifel … the Eifel Plume …

… Our findings suggest that the surface deformation imposed by the Eifel plume explains why
… (such as the Upper Rhine Graben (URG) between the Eifel and Alps). In fact, we see no …