Implications of Detrital Shocked Minerals at the Mouth of the Orange River: Continental Scale Transport by Fluvial, Eolian, and Coastal Processes

Details Implications of Detrital Shocked Minerals at the Mouth of the Orange River: Continental Scale Transport by Fluvial, Eolian, and Coastal Processes Implications of Detrital Shocked Minerals at the Mouth of the Orange River: Continental Scale Transport by Fluvial, Eolian, and Coastal Processes

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.1938e&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.1938

Physics

Scientific paper

We document detrital shocked grains from the mouth of the Orange River
in South Africa. These grains require long (1200 to 2000 km) distances
of transport, diverse sedimentary processes, and originate from multiple
impact basins.

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