Preferred Mineral Orientations in Martian Shergottites: Magmatism or Schock?
We have studied the textures and the preferred orientation of pyroxene in subsamples of Zagami and Nakhla using Electron Backscatter Diffraction (EBSD) method. Data show the activation of several slip systems, related to magmatism or shock event.
| Main Authors: | , , , |
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| Format: | Conference Paper |
| Published: |
WILEY-BLACKWELL
2012
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| Online Access: | http://www.lpi.usra.edu/meetings/metsoc2012/pdf/5145.pdf http://hdl.handle.net/20.500.11937/47563 |