Experimental Shock Metamorphism of Terrestrial Basalts Induced by Shock Waves up to 115 GPa: Agglutinate-Like Particles' Formation, Petrology and Magnetism

Details Experimental Shock Metamorphism of Terrestrial Basalts Induced by Shock Waves up to 115 GPa: Agglutinate-Like Particles' Formation, Petrology and Magnetism Experimental Shock Metamorphism of Terrestrial Basalts Induced by Shock Waves up to 115 GPa: Agglutinate-Like Particles' Formation, Petrology and Magnetism

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.2826b&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.2826

Physics

Scientific paper

We investigated particles that were found in products from high-velocity
shock experiments with peak shock pressures up to 115 GPa. Texturally,
the particles are similar to lunar agglutinates. The particles have
specific magnetic characteristics.

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