The Origin of Chondrites: Metal-Silicate Separation Experiments Under Microgravity Conditions

Details The Origin of Chondrites: Metal-Silicate Separation Experiments Under Microgravity Conditions The Origin of Chondrites: Metal-Silicate Separation Experiments Under Microgravity Conditions

Mar 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003lpi....34.1046m&link_type=abstract

34th Annual Lunar and Planetary Science Conference, March 17-21, 2003, League City, Texas, abstract no.1046

Physics

Scientific paper

The metal/silicate ratio is a distinctive attribute of the meteorite
classes. Here, we describe the results of fluidization experiments in
microgravity, showing that separation of metal and silicate grains
occurs readily, and we suggest that this could occur on parent bodies.

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