Electron backscatter diffraction data for samples from natural upper mantle shear zones in the Josephine Peridotite, SW Oregon
- Kumamoto, Kathryn M
- Warren, Jessica M
- Hansen, Lars N
To understand how olivine microstructures evolve with increasing strain during upper mantle deformation, we analyzed a suite of natural peridotite shear zone samples using electron backscatter diffraction. For each sample, we produced a map of mineral orientations, recorded in a Channel Text File (.ctf). Each row of data represents one pixel of the map. Indexed phases typically include olivine, orthopyroxene, clinopyroxene, chromite, and tremolite.
How to cite this dataset:
Kumamoto, K., Warren, J., Hansen, L. 2019. Electron backscatter diffraction data for samples from natural upper mantle shear zones in the Josephine Peridotite, SW Oregon, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.1594/IEDA/111365.
DOI Creation Date:
Kumamoto, K.M., Warren, J.M. and Hansen, L.N., 2019. Evolution of the Josephine Peridotite Shear Zones: 2. Influences on Olivine Cpo Evolution. Journal of Geophysical Research: Solid Earth, 124(12), pp.12763-12781.
Creative Commons Attribution-ShareAlike 4.0 International [CC BY-SA 4.0]
- National Science Foundation: 1255620
- National Science Foundation: 1625032
- Coverage Scope: Regional (Continents, Oceans)
- Geographic Location: Josephine Peridotite, SW Oregon
User Contributed Keyword(s):
rheology, upper mantle, shear zone, crystal-preferred orientation, lattice-preferred orientation, EBSD
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