Lunar Impact-fluidized Dikes: Evidence from Apollo 17 Station 7, Taurus-Littrow Valley

Details Lunar Impact-fluidized Dikes: Evidence from Apollo 17 Station 7, Taurus-Littrow Valley Lunar Impact-fluidized Dikes: Evidence from Apollo 17 Station 7, Taurus-Littrow Valley

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.1176h&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.1176

Computer Science

Scientific paper

3-5 cm wide dikes intruding noritic breccia at the Apollo 17 station 7
boulder comprise angular mineral and lithic clasts. The dikes are not
igneous. They were generated by vapour-fluidized comminuted material and
lithified by condensing silicate vapours and/or by subsequent shock
welding.

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