UC Santa Cruz Previously Published Works Let us know how this
gation [Nielsen and Knopoff, 1998; Aochi and Madariaga, 2003] and the close relationship between the rupture geome-try and its propagation velocity [Vallée et al , 2008; Bouchon et al ,2010] [3] As direct observations are not possible at the depths of earthquake nucleation, surface roughness data from
On the origin of falling-tone chorus elements in Earth’s
ing 2002–2003 was found to be ˘200km at Lˇ4:4 (San-tolík and Gurnett,2003), ˘600km at Lˇ5 (Agapitov et al , 2011a) and ˘3000km for Lˇ8–9 (Agapitov et al ,2010) A secondary source may lie in pockets of minimum mag-netic field at high-latitude in the dayside magnetosphere (Tsurutani and Smith,1977;Keika et al ,2012) during high
Shear wave propagation in jointed rock: state of stress
Fratta, D & Santamarina, J C (2002) Ge´otechnique 52, No 7, 495–505 Shear wave propagation in jointed rock: state of stress D FRATTA and J C SANTAMARINA{The mechanical characteristics and orientation of joints determine the behaviour of rock masses, including the strength, the stiffness, and all forms of conduction and diffusion
Cooperativity in two-state protein folding kinetics
Cooperativity in two-state protein folding kinetics THOMAS R WEIKL,1,2 MATTEO PALASSINI,1,3 AND KEN A DILL1 1 Department of Pharmaceutical Chemistry, University of California, San Francisco, California 94143, USA
NATIONS UNIES ANNUAIRE JURIDIQUE
4 Décision n° 301 (19 juillet 2003) : c LavelleBanque internationale pour la reconstruction et le développement — Retraites et régime des retraites — Conditions à remplir pour pouvoir bénéficier d’une re-traite — Personnel d’appoint — Règles générales — Différenciation
EXERCICES ET PROBLÈMES D’ÉLECTROTECHNIQUE
D u n o d – L a p h o t o c o p i e qui ont contribu n o n a u t o r i s é e e s t u n d é l i t Avant propos Cet ouvrage regroupe 7 synthèses de cours, 38 exercices corrigés et 11 problèmes,
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