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- W2054857616 abstract "The Flims sturzstrom deposit (Swiss Alps) is the largest in the Alps (12 km3, H/L = 0.13). It consists of stratified breccias that display planar discontinuities that originated during transport. Major sliding surfaces are underlined by frictional gouge. Between these surfaces, the material is fragmented with rotated fault blocks bordered by oblique fractures that show the transport directions. The transport mechanisms of the debris avalanche were dominated by layer-parallel slip movements that favoured the nonturbulent behaviour of the granular material and the reduction of internal friction. Les dépôts du sturzstrom de Flims (Alpes suisses) sont les plus volumineux des Alpes (12 km3, H/L = 0,13). Ils correspondent à des brèches stratifiées, qui présentent des discontinuités planaires, dont l'origine est liée au mode de transport des matériaux. Les surfaces majeures de glissement sont soulignées par des horizons fortement cataclasés. Elles emballent des matériaux fragmentés par des fractures obliques, dont l'orientation témoigne d'une rotation des clastes, et matérialisent les directions d'écoulement. Le transport de l'avalanche de débris est dominé par des mouvements couche sur couche favorables à un comportement non turbulent de la masse granulaire et à la réduction de la friction interne." @default.
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- W2054857616 date "1999-05-01" @default.
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- W2054857616 title "La fabrique interne des dépôts du sturzstrom de Flims (Alpes suisses): caractéristiques et implications sur les mécanismes de transport" @default.
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- W2054857616 doi "https://doi.org/10.1016/s1251-8050(99)80157-8" @default.
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