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  • La diagonal arida argentina: un limite climatico real
  • Husbands' and wives' characteristics and fertility decisions : a diagonal mobility model
  • D'après le modèle diagonal de Sobel, la fécondité varie en fonction d'effets pondérés provenant de caractéristiques liées à l'éducation des époux et des épouses. Importance des stéréotypes ethniques. Application aux Etats-Unis (Arizona, Nouveau
  • Increasing the efficiency of pooled estimation with a block-diagonal covariance structure
  • Arrays of flow data are, statistically, difficult to analyse because the definition of diagonal terms. Using an example of a commercial input-output table, a similarity index is defined. It is shown that this index allows a hierarchical clustering
  • This article briefly summarises the plane Euclidian representation of the set of tables associated with a symmetrical table and its margins (tables which differ in particular in respect to the relative wheights of the diagonals) and direct
  • The main watershed in Bulgaria follows the Diagonal Swell, the young geological structure having affected the geodynamic processes during the neotectonic period. - (SBV)
  • Reconstruction of an approximately complete Quaternary Tibetan inland glaciation between the Mt. Everest- and Cho Oyu Massifs and the Aksai Chin. A new glaciogeomorphological SE-NW diagonal profile through Tibet and its consequences for the glacial
  • Distribution of mountain protected areas of the Andean Cordillera and the extent of the arid diagonal, the zone from SW Ecuador to eastern Argentina, are compared. Authors find very few mountains protected areas in the most arid ecosystems, from
  • of the ocean bottom relief. There are three types of motions, namely vertical (subsidence) at mid-oceanic ridges, horizontal (moving apart) at continental terraces and diagonal motions (down and apart from the ridge axis) within abyssal plains. Progressive
  • methodology. More than 120 fluvial basins were studied. There are 2 large hydrological regions, the Western and the Eastern, with a northeastern transverse diagonal boundary, coinciding with the direction of the Beta Escarpment. Using quantitative data
  • model (DEM) of southern Norway and a 2m LiDAR DSM of the Lake District, UK. Both datasets contained diagonal data artefacts. Spectral filtering used fast Fourier transformation (FFT) frequency data to identify these data artefacts in both datasets