Excess 40Ar in Martian Shergottites, K-40Ar Ages of Nakhlites, and Implications for In Situ K-Ar Dating of Mars' Surface Rocks

Details Excess 40Ar in Martian Shergottites, K-40Ar Ages of Nakhlites, and Implications for In Situ K-Ar Dating of Mars' Surface Rocks Excess 40Ar in Martian Shergottites, K-40Ar Ages of Nakhlites, and Implications for In Situ K-Ar Dating of Mars' Surface Rocks

Mar 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008lpi....39.1100b&link_type=abstract

39th Lunar and Planetary Science Conference, (Lunar and Planetary Science XXXIX), held March 10-14, 2008 in League City, Texas.

Physics

1

Scientific paper

Martian shergottites contain similar concentrations of excess
40Ar inherited from the magma; six martian nakhlites contain
little excess 40Ar and define an isochron age of 1325 m.y.;
K-Ar dating on Mars will require rocks with varying K concentrations.

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