Microstructure and Crystallographic Preferred Orientations of an Azimuthally Oriented Ice Core from a Lateral Shear Margin: Priestley Glacier, Antarctica

A 58 m long azimuthally oriented ice core has been collected from the floating lateral sinistral shear margin of the lower Priestley Glacier, Terra Nova Bay, Antarctica. The crystallographic preferred orientations (CPO) and microstructures are described in order to correlate the geometry of anisotro...

ver descrição completa

Detalhes bibliográficos

Principais autores:	Rilee E. Thomas, Marianne Negrini, David J. Prior, Robert Mulvaney, Holly Still, M. Hamish Bowman, Lisa Craw, Sheng Fan, Bryn Hubbard, Christina Hulbe, Daeyeong Kim, Franz Lutz
Formato:	Artigo
Idioma:	Inglês
Publicado em:	Frontiers Media S.A. 2021-11-01
coleção:	Frontiers in Earth Science
Assuntos:	lateral glacial shear margin crystallographic preferred orientations ice microstructure ice deformation and flow electron backscatter diffraction Priestley Glacier
Acesso em linha:	https://www.frontiersin.org/articles/10.3389/feart.2021.702213/full
Tags:	Adicionar Tag Sem tags, seja o primeiro a adicionar uma tag!