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  • 1995-1999  (2)
  • 1900-1904
  • Anterior disk displacement  (1)
  • SW Urals  (1)
  • 1
    ISSN: 1432-2102
    Keywords: Schlüsselwörter MRT ; Kiefergelenk ; Diskusverlagerung ; Morphometrie ; Key words MRI ; Temporomandibular joint ; Anterior disk displacement ; Metric analysis
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Description / Table of Contents: Summary In order to evaluate magnetic resonance imaging (MRI) changes in correlation with different degrees of internal derangement of the temporomandibular joint, we evaluated 117 joints of 59 symptomatic patients and 31 volunteers. Data analysis included morphologic and morphometric characteristics. Sixteen joints (19 %) were considered normal, 40 demonstrated anterior displacement with reduction (47 %) and 27 anterior displacement without reduction (32 %). In three of the volunteers anterior displacement with reduction was noted. Advancing anterior position of the disk was associated with reduced ability to open the mouth, progressive deformity and shortening of the disk, thinning of the bilaminar zone, regressive and proliferative bony changes of the condyle, reduced translatory movement of the disk and condyle, thinning of joint space, cranial and dorsal displacement of the condyle and flattening of the slope of the tuberculum. In addition to alterations in condylar and disk morphology, MRI can demonstrate various additional measurable changes that correlate well with the degree of anterior disk displacement.
    Notes: Zusammenfassung Um den Einfluß der Diskusverlagerung im Kiefergelenk auf die Gelenkbinnenstrukturen zu untersuchen, wurden insgesamt 117 Gelenke von 59 symptomatischen Patienten und 31 asymptomatischen Probanden in der MRT untersucht und die Gelenkbinnenstrukturen sowohl morphologisch wie morphometrisch beurteilt. Im Patientengut lag 16mal eine normale Diskusposition (NDP) (19 %), 40mal eine Vorverlagerung mit Reposition (VMR) (47 %) und 27mal eine Vorverlagerung ohne Reposition (VOR) (32 %) vor. Unter den Normalpersonen zeigten 3 eine VMR. Mit zunehmender Diskusvorverlagerung zeigte sich eine kleiner werdende maximale Mundöffnung, ein zunehmend deformierter und verkürzter Diskus, eine Ausdünnung der bilaminären Zone, eine Abnahme des Durchmessers und zunehmende Entrundung des Processus condylaris, eine verminderte translatorische Diskus- und Kondylusbeweglichkeit, eine Verschmälerung der Gelenkspaltweite, eine Verlagerung des Processus condylaris in geschlossener Mundposition nach kranial und dorsal und eine Abflachung des Kondylenbahnwinkels. Neben der Morphologie des Diskus und Kondylus bzw. deren Morphologie lassen sich damit eine ganze Reihe weiterer magnetresonanztomographisch quantifizierbarer Befunde im Rahmen von Verlagerungen des Diskus im Temporomandibulargelenk darstellen.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 0016-7835
    Keywords: Key words Structural analysis ; Bashkirian anticlinorium ; SW Urals ; URSEIS '95 profile
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The Bashkirian anticlinorium of the southwestern Urals shows a much more complex structural architecture and tectonic evolution than previously known. Pre-Uralian Proterozoic extensional and compressional structures controlled significantly the Uralian tectonic convergence. A long-lasting Proterozoic rift process created extensional basement structures and a Riphean basin topography which influenced the formation of the western fold-and-thrust-belt with inversion structures during the Uralian deformation. A complete orogenic cycle during Cadomian times, including terrane accretion at the eastern margin of the East European platform, resulted in a high-level Cadomian basement complex, which controlled the onset of Uralian deformation, and resulted in intense imbrication and tectonic stacking in the subjacent footwall of the Main Uralian fault. The Uralian orogenic evolution can be subdivided into three deformation stages with differently oriented stress regimes. Tectonic convergence started in the Late Devonian with ophiolite obduction, tectonic accretion of basin and slope units and early flysch deposits (Zilair flysch). The accretionary complex prograded from the SE to the NW. Continuous NW/SE-directed convergence resulted finally in the formation of an early orogenic wedge thrusting the Cadomian basement complex onto the East European platform. The main tectonic shortening was connected with these two stages and, although not well constrained, appears to be of Late Devonian to Carboniferous age. In the Permian a final stage of E–W compression is observed throughout the SW Urals. In the west the fold-and-thrust-belt prograded to the west with reactivation of former extensional structures and minor shortening. In the east this phase was related to intense back thrusting. The East European platform was subducted beneath the Magnitogorsk magmatic arc during the Late Paleozoic collision. The thick and cold East European platform reacted as a stable rigid block which resulted in a narrow zone of intense crustal shortening, tectonic stacking and high strain at its eastern margin. Whereas the first orogenic wedge is of thick-skinned type with the involvement of crystalline basement, even the later west-directed wedge is not typically thin-skinned as the depth of the basal detachment appears below 15 km and the involvement of Archean basement can be assumed.
    Type of Medium: Electronic Resource
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