Conditions for thrust faulting in a glacier

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چکیده

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Conditions for Thrust Faulting in a Glacier

Dipping, arcuate bands of debris-rich ice outcropping near the margins of glaciers are often interpreted as thrust faults, assumed to originate in zones of longitudinal compression. Identification of thrusts is typically based either on the geometry and sedimentology of the debris bands or on the crystal fabric of surrounding ice, but the physical processes necessary to generate thrusts are rar...

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ژورنال

عنوان ژورنال: Journal of Geophysical Research: Earth Surface

سال: 2010

ISSN: 0148-0227

DOI: 10.1029/2009jf001307