Preferred slip-band orientations and bending observed in the Dome Concordia (East Antarctica) ice core

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Preferred slip band orientations and bending observed in the Dome Concordia ice core

Fabric analysis of the upper 1300m of the Dome C ice core reveals a slight clustering tendency of c axes towards vertical, which gradually enhances with depth from an initially isotropic orientational distribution of c axes at the free surface. Such a strain induced anisotropy is compatible with the expected macroscale stress state in a dome, viz. dominated by vertical compression. Yet, when on...

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1 Laboratoire de Glaciologie et Géophysique de l’Environnement, CNRS and Joseph Fourier University, Grenoble, France 2 Laboratoire des Sciences du Climat et de l’Environnement, Gif-Sur-Yvette, France 3 Niels Bohr Institute for Astronomy, Physics and Geophysics, Copenhagen, Denmark 4 National Institute of Polar Research, Research Organization of Information and Systems (ROIS), Tokyo, Japan 5 Cen...

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ژورنال

عنوان ژورنال: Annals of Glaciology

سال: 2004

ISSN: 0260-3055,1727-5644

DOI: 10.3189/172756404781814078