Determining the Impactor of the Ordovician Lockne Crater: Oxygen Isotopes in Chromite versus Sedimentary Pge

نویسندگان

  • SIGNATURES B. Schmitz
  • P. R. Heck
  • C. Alwmark
  • N. T. Kita
  • B. Peucker-Ehrenbrink
  • T. Ushikubo
چکیده

IN CHROMITE VERSUS SEDIMENTARY PGE SIGNATURES B. Schmitz , P. R. Heck, C. Alwmark, N. T. Kita, B. Peucker-Ehrenbrink, T. Ushikubo, and J. W. Valley, Department of Geology, Sölvegatan 12, Lund University, SE-22362 Lund, Sweden, [email protected], Department of Geology and Geophysics, University of Wisconsin, 1215 W. Dayton St., Madison, WI 53706, USA, Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA.

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Determining the impactor of the Ordovician Lockne crater: Oxygen and neon isotopes in chromite versus sedimentary PGE signatures

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تاریخ انتشار 2009