Shock metamorphism on the ocean floor (numerical simulations)

@article{Artemieva2002ShockMO,
  title={Shock metamorphism on the ocean floor (numerical simulations)},
  author={N. Artemieva and V. Shuvalov},
  journal={Deep-sea Research Part Ii-topical Studies in Oceanography},
  year={2002},
  volume={49},
  pages={959-968}
}
  • N. Artemieva, V. Shuvalov
  • Published 2002
  • Geology
  • Deep-sea Research Part Ii-topical Studies in Oceanography
  • Abstract Impact craters are unknown in deep-ocean basins. Important reasons for this are that the ocean crust is younger than continents and the impacts are weakened by the water column. Laboratory experiments can show specific features of water impacts. However, impact velocities are too small ( 
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    References

    SHOWING 1-10 OF 22 REFERENCES
    Melt Production in Oblique Impacts
    • 175
    • PDF
    First Natural Occurrence of Coesite
    • 222