Calcul du Montant Original des Nombres Décimaux et des Pourcentages Variant de 1 à 99 (A)

These flexural modeling constraints refute the existence of a negligible relief in the northern Tibetan pla- teau during the Paleogene (Meyer et al.,  1998 ; Tapponnier et al.,  2001

A, Organisation de la séquence génétique (c'est-à-dire le plus petit cycle de variation du niveau de base) : en période de régression (demi-cycle régressif), l'accomodation

et al., 1995; Valente et al., 1997) have been applied to subtropical mixed forest in China. Shaoshan forest is with two-layer canopy structure, i.e. It is di fficult to predict

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2 the 2002–2003 statistics estimations are given for the reliability of the time window earthquake prediction on the basis of geomagnetic field measurements (Mavrodiev, 2002b) and

The proposed GSDW model will have the ability to simulate relevant hydrological processes, e.g., canopy interception, evapo- transpiration, surface runoff, lateral

Weighted average δ 18 O p values for the three sites over the common time period April 2005 to September 2006 (not including August and September 2005 for all sites, as there was

plained by the near-bed hydraulic variables Vx and σVx implies that there is a degree of active or passive selection of hydraulic conditions by benthic invertebrates that occurs