DataSheet1_Microstructure and Crystallographic Preferred Orientations of an Azimuthally Oriented Ice Core from a Lateral Shear Margin: Priestley Glacier, Antarctica.PDF

• Main Authors: 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
• Format: Dataset
• Language: unknown
• Published: 2021
• Subjects: Solid Earth Sciences; Climate Science; Atmospheric Sciences not elsewhere classified; Exploration Geochemistry; Inorganic Geochemistry; Isotope Geochemistry; Organic Geochemistry; Geochemistry not elsewhere classified; Igneous and Metamorphic Petrology; Ore Deposit Petrology; Palaeontology (incl. Palynology); Structural Geology; Tectonics; Volcanology; Geology not elsewhere classified; Seismology and Seismic Exploration; Glaciology; Hydrogeology; Natural Hazards; Quaternary Environments; Earth Sciences not elsewhere classified; Evolutionary Impacts of Climate Change; lateral glacial shear margin; crystallographic preferred orientations; ice microstructure; ice deformation and flow; electron backscatter diffraction; Priestley Glacier; Terra Nova Bay; Priestley; Antarc*; Antarctica; ice core
• Online Access: https://doi.org/10.3389/feart.2021.702213.s001; https://figshare.com/articles/dataset/DataSheet1_Microstructure_and_Crystallographic_Preferred_Orientations_of_an_Azimuthally_Oriented_Ice_Core_from_a_Lateral_Shear_Margin_Priestley_Glacier_Antarctica_PDF/17084660

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...