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  • 1
    Electronic Resource
    Electronic Resource
    Woodbury, NY : American Institute of Physics (AIP)
    Chaos 6 (1996), S. 43-58 
    ISSN: 1089-7682
    Source: AIP Digital Archive
    Topics: Physics
    Notes: The billiard system of Benettin and Strelcyn [Phys. Rev. A 17, 773–785 (1978)] is generalized to a two-parameter family of different shapes. Its boundaries are composed of circular segments. The family includes the integrable limit of a circular boundary, convex boundaries of various shapes with mixed dynamics, stadiums, and a variety of nonconvex boundaries, partially with ergodic behavior. The extent of chaos has been measured in two ways: (i) in terms of phase space volume occupied by the main chaotic band; and (ii) in terms of the Lyapunov exponent of that same region. The results are represented as a kind of phase diagram of chaos. We observe complex regularities, related to the bifurcation scheme of the most prominent resonances. A detailed stability analysis of these resonances up to period six explains most of these features. The phenomenon of breathing chaos [Nonlinearity 3, 45–67 (1990)]—that is, the nonmonotonicity of the amount of chaos as a function of the parameters—observed earlier in a one-parameter study of the gravitational wedge billiard, is part of the picture, giving support to the conjecture that this is a fairly common global scenario. © 1996 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 1996-03-01
    Print ISSN: 1054-1500
    Electronic ISSN: 1089-7682
    Topics: Physics
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  • 3
    Publication Date: 2021-03-29
    Description: The suevitic Onaping Formation overlies the layered Main Mass of the 1.85Ga Sudbury Igneous Complex (SIC) of the Sudbury Impact Structure, Ontario. The Formation consists of four Members, namely from top to bottom, the Black, the Green, the Gray and the Basal. Post-impact NWSE shortening during the Penokean Orogeny (ca. 1.9–1.75 Ga) affected the Onaping Formation and led to the lobate shape of the SIC in plan view. In order to investigate the possible fold origin of the NE-lobe of the SIC, a field-based structural analysis of the Onaping Formation was conducted in the Frenchman Lake area. The analysis is based on structural measurements at 580 stations and encompasses the orientation of mineral shape fabrics as well as their intensity. In addition to these quantities, lithological variation and metamorphic overprint of the Onaping Formation was examined. Special attention was paid thereby to the Green Member since previous workers stated that it forms a continuous unit at the base of the Black Member...
    Description: conference
    Keywords: 551 ; VKB 280 ; VKB 295 ; VAE 140 ; VEV 127 ; VKA 200 ; Impaktgesteine {Petrologie} ; Metamorphe Komplexe, Nordamerika {Petrologie} ; Gesteinsdeformation {Strukturgeologie} ; Ontario {Geologie} ; Gefügekunde der Gesteine ; Sudbury 〈Ontario. Region〉 ; Mehrfachringbassin ; Proterozoikum ; Impaktmetamorphes Gestein ; Suevit ; Deformation 〈Geologie〉
    Language: German
    Type: anthologyArticle , publishedVersion
    Format: application/pdf
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