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  • Artikel: DFG Deutsche Nationallizenzen  (2)
  • 1990-1994  (2)
  • 1970-1974
  • 68,35.Fx  (1)
  • Neotectonics  (1)
Datenquelle
  • Artikel: DFG Deutsche Nationallizenzen  (2)
Materialart
Erscheinungszeitraum
  • 1990-1994  (2)
  • 1970-1974
Jahr
  • 1
    Digitale Medien
    Digitale Medien
    Springer
    International journal of earth sciences 82 (1993), S. 67-83 
    ISSN: 1437-3262
    Schlagwort(e): Neotectonics ; central Europe ; northern Europe
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Geologie und Paläontologie
    Notizen: Abstract The ‘neotectonic period’ is the youngest period of tectonic evolution and extends up to the present. The beginning of the neotectonic period during the Cenozoic may be regarded as having begun when characteristic changes in the tectonic evolution of a region of interest have occurred for the last time. Changes in the different tectonic facets, which characterize the evolution of a region, need not be simultaneous, and hence the times of the last change may differ between facets. This leads to the definition of a ‘transitional time interval’ wherein elements of both the ‘palaeotectonic’ and neotectonic period are present. The length of this transitional time interval depends on the regional geological evolution. Where a broad transitional time interval exists, the beginning of the neotectonic period may be defined by the earliest time marker by when most of the characteristic changes of the tectonic evolution of the region had occurred. In defining the neotectonic period in central and northern Europe, data on the evolution of the northern Mid-Atlantic ridge and the northern Mediterranean convergence zone, inversion tectonics in northern and central Europe, rifting, regional subsidence and uplift, and the tectonic stress field as well as the evolution of the calcalkaline and alkaline volcanism in central Europe have been taken into account. The chronological evolution of these ‘characteristics’ for the Cenozoic have been analysed with a view to identifying the advent of the neotectonic period. The transition from the end of the palaeotectonic period to the beginning of the neotectonic period extends from the middle early Miocene to the Miocene-Pliocene boundary. The earliest time by when most of the characteristic changes in the tectonic evolution of northern and central Europe had occurred is the early late Miocene. Thus, the neotectonic period can be considered to have begun at approximately 10 Ma before present.
    Materialart: Digitale Medien
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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  • 2
    Digitale Medien
    Digitale Medien
    Springer
    Applied physics 53 (1991), S. 369-376 
    ISSN: 1432-0630
    Schlagwort(e): 68.55.−a ; 68,35.Fx ; 61.16.Fk
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Maschinenbau , Physik
    Notizen: Abstract The growth of Pt(111) by Pt vapour deposition is studied by He diffraction as a function of substrate temperature and deposition rate. At a deposition rate of about 2.5×10−2 monolayers/second several growth modes are observed: layer-by-layer (2D-) growth at 450 K≲T s≲800 K, multilayer (3D-) growth at 340 K≲T s≲450 K and reentrant layer-by-layer (2D-) growth at T s≲340 K. The observed growth modes and in particular the reentrant 2D-growth are shown to be characteristic of growing Pt(111) under clean conditions, i.e. not influenced by contaminants. The influence of the intra- and interlayer mass transport on the growth mode is discussed in the light of experimental and simulation results. The 3D-growth mode is attributed to the existence of an activation barrier which suppresses the descent of adatoms from the top of the growing adatom islands onto the lower terraces. The barrier can be overcome by thermal adatoms at T s≳450 K enabling interlayer mass transport which leads to 2D-growth. The reentrant 2D-growth occurs due to a break down of this barrier for small, irregularly shaped islands.
    Materialart: Digitale Medien
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
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