Nanoscale records of ancient shock deformation: Reidite (ZrSiO4) in sandstone at the Ordovician Rock Elm impact crater
The terrestrial record of meteorite impacts is difficult to decipher because unequivocal evidence of impact is increasingly destroyed with time by erosion, burial, and tectonics. Zircon survives these processes as a shocked mineral, and above 20 GPa transforms to reidite, a high-pressure ZrSiO4 poly...
| Main Authors: | , , |
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| Format: | Journal Article |
| Published: |
GEOLOGICAL SOC AMER, INC
2015
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| Online Access: | http://hdl.handle.net/20.500.11937/11281 |
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