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In geology oblique foliation, steady state foliation or oblique fabric is a special type of a tectonically produced foliation or fabric, most commonly in quartz-rich layers. The structure can be used to determine the shear sense in shear zones and their associated rocks, usually mylonites.

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  • Schräge Foliation (de)
  • Foliation oblique (fr)
  • Oblique foliation (en)
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  • Schräge Foliation oder schräges Gefüge ist eine während des tektonischen Verformungsprozesses entstehende spezielle Art von Foliation. Dieses Gefüge tritt hauptsächlich in quarzreichen Lagen von Myloniten auf. Es wird in der , einem Teilgebiet der Strukturgeologie, zur Bestimmung des jeweiligen Schersinns verwendet. (de)
  • In geology oblique foliation, steady state foliation or oblique fabric is a special type of a tectonically produced foliation or fabric, most commonly in quartz-rich layers. The structure can be used to determine the shear sense in shear zones and their associated rocks, usually mylonites. (en)
  • La foliation oblique ou texture oblique est une foliation/texture spéciale produite pendant la déformation cisaillante. Elle est bien exprimée dans les lits quartzeux des mylonites. En cette structure sert à déterminer le sens de dans le les zones de cisaillement. (fr)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/ObliqueFoliation.jpg
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  • Schräge Foliation oder schräges Gefüge ist eine während des tektonischen Verformungsprozesses entstehende spezielle Art von Foliation. Dieses Gefüge tritt hauptsächlich in quarzreichen Lagen von Myloniten auf. Es wird in der , einem Teilgebiet der Strukturgeologie, zur Bestimmung des jeweiligen Schersinns verwendet. (de)
  • In geology oblique foliation, steady state foliation or oblique fabric is a special type of a tectonically produced foliation or fabric, most commonly in quartz-rich layers. The structure can be used to determine the shear sense in shear zones and their associated rocks, usually mylonites. (en)
  • La foliation oblique ou texture oblique est une foliation/texture spéciale produite pendant la déformation cisaillante. Elle est bien exprimée dans les lits quartzeux des mylonites. En cette structure sert à déterminer le sens de dans le les zones de cisaillement. (fr)
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