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1979-05-01
Elastic Waves in the Earth - de Walter L. Pilant (Author)
Caractéristiques Elastic Waves in the Earth
Les données suivantes répertorie les spécificités utiles du Elastic Waves in the Earth
| Le Titre Du Fichier | Elastic Waves in the Earth |
| Sortié Le | 1979-05-01 |
| Traducteur | Savanha Easa |
| Nombre de Pages | 850 Pages |
| Taille du fichier | 37.23 MB |
| Langage | Français et Anglais |
| Éditeur | Vine Press |
| ISBN-10 | 2508335341-ZSQ |
| Type de Fichier | AMZ EPub PDF LBR SXW |
| Écrivain | Walter L. Pilant |
| EAN | 867-6254889031-QFO |
| Nom de Fichier | Elastic-Waves-in-the-Earth.pdf |
Télécharger Elastic Waves in the Earth Livre PDF Gratuit
Meilleure réponse Pwaves are a type of elastic wave also called seismic waves that can travel through gasses such as sounds elastic solids and liquids including the Earth Pwaves can be produced by earthquakes and recorded by seismometers The name Pwave stands for primary wave as the P
Traductions en contexte de utilisé pour générer en françaisanglais avec Reverso Context peut être utilisé pour générer
Elastic deformation at short time scale normal modes solid Earth tides Love numbers ocean and atmosphere loading Chandler wobble Viscoelastic deformation at long time scale postglacial rebound
misfit function the surface wave energy usually masks the body waves and the gradient of the misfit function exhibits high values in the very shallow depths preventing from recovering the deeper part of the earth model parameters
Wu R and K Aki 1985 Scattering characteristics of elastic waves by an elastic heterogeneity Frankel A and Clayton 1986 Finite difference simulations of seismic scattering implications for the propagation of shortperiod seismic waves in the crust and models of crustal heterogeneity Res 91 64656489
The evolution of elastic anisotropy was quantified using Thomsens parameters which were directly inverted from measurement of elastic wave velocity Brittle failure was preceded by a change in P wave anisotropy due to both crack growth and mineral reorientation Anisotropy variations were largest for samples deformed perpendicular to bedding at the onset of rupture Anisotropy reversal was
Highresolution seismic imaging is essential to improve results of hydrocarbon waves propagate in the Earth as body and surface waves the latter being the mostenergetic ones Body waves are preferred for exploration seismic imaging while surfacewaves are usually considered to be noise However it has been recognised that the nearsurface can be characterised by analysing