Abstract
In the Earth's middle and lower crust and mantle, rocks deform by creep, and it has long been recognized that lattice preferred orientations1 (LPO) of the mineral constituents in deformed rocks yield useful information on creep deformation mechanisms, conditions, and kinematics (Leiss et al. 2000; Turner and Weiss 1963;Wenk and Christie 1991). Bulk LPO data are traditionally measured by X-ray texture goniometry, and more recently using neutron and synchrotron sources (Leiss et al. 2000). © Springer Science+Business Media, LLC 2009. All rights reserved.
Cite
CITATION STYLE
Prior, D. J., Mariani, E., & Wheeler, J. (2009). EBSD in the earth sciences: Applications, common practice, and challenges. In Electron Backscatter Diffraction in Materials Science (pp. 345–360). Springer US. https://doi.org/10.1007/978-0-387-88136-2_26
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.
