Slip rate and mode of the Feldbiss normal fault (Roer Valley Graben) after removal of groundwater effects

However, modeling saltation intermittency from a LES approach is still chal- lenging because saltation occurs near the surface, within a layer not exceeding 1 m height, where

It has been established that this defects is related to the change in mineralization form from hexagonal aragonite to orthorhombic vaterite.. SEM picture of pearl surface at

Note that, if stress shadowing had not been included in our calcu- lations, the weakening functions above would not have succeeded alone in reproducing the observed slip profiles;

a) Schematic view of damaged zone deformation near active fault: earthquake-induced fracturing networks (black) that are progressively sealed by self-healing and sealing

Along the North Ih Bogd segment, we estimated the horizontal slip rate of the Bogd Fault at Bitut, a site located 40 km east of the the Noyan Uul site (Fig.. There, a system of

In addition, in their extended analysis of spatial correlations of slip maps for 44 earthquakes, Mai & Beroza (2002) found that the heterogeneous slip distribution follows

(D) and (E) show close-ups of the base of the fault free-plane (location shown in A, B, and C), showing a ribbon of slip surface exposed during the 2004 seismic event (coseismic

Slip rate of trench-parallel normal faulting along the Mejillones Fault (Atacama Fault System): Relationships with the northern Chile subduction and implications for seismic