This suggests that a correct interpretation of the P-wave velocity measured from borehole sonic logging needs to consider the effect of borehole stress concentration which results in
The variations in the wave- length for the layer thickness clearly illustrate the im- portance of mechanical layering and of the coupling between different layers in the deformation
The present work intends to verify experimentally that pressure stimulated current emissions in amphibolite, pro- duced by loading-unloading procedures that are based on abrupt uniaxial
To study properties of compressional wave events in the dawn plasma sheet, the authors provided an analysis of plasma and magnetic ®eld measurements in the middle tail of the Earth
The increase in trilobite size from shallow 293 proximal to deep distal localities in the Fezouata Shale is consistent with observations of 294 crustacean body size
Comparison of horizontal deviatoric stress between the forced subduction model (panels a-c) and the free.
24 disciplines dans le second degré 1200 étudiants en M1 500 étudiants en M2 400 étudiants en DU 600 lieux de stage en M1 45 sites de formation 6 universités partenaires.2.
Our integrated approach includes 1) epidemiological studies (investigate the presence of African swine fever, cysticercosis, hepatitis E, and internal parasites in blood samples, organs
Based on 2400 terms extracted with the text-mining approach, our automatic search system associated with the collective domain expertise (i.e. evaluation of 20 groups of terms by 21
Overall, 144 combinations of 12 offtake patterns (varying Tabaski month) with 12 vaccination months were assessed with 3 indicators: i) number of months with immunity coverage > 80%,
EC w values (S.cm -1 ) during rice plant cultivation. Calibration curves for 2AP in leaves matrix. Calibration curves for 2AP in grain matrix ……….. Schematic representation of
We have shown that assuming a deformed mean field model or taking account of two- body correlations in a spherical model leads to close results for the inversion of 1/2 +.