4.8 Article

Unique Meteorite from Early Amazonian Mars: Water-Rich Basaltic Breccia Northwest Africa 7034

Journal

SCIENCE
Volume 339, Issue 6121, Pages 780-785

Publisher

AMER ASSOC ADVANCEMENT SCIENCE
DOI: 10.1126/science.1228858

Keywords

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Funding

  1. NASA Cosmochemistry Program [NNX11AH16G, NNX11AG76G]
  2. New Mexico Space Grant Consortium
  3. NASA Earth and Space Science Fellowship [NNX12AO15H]
  4. NASA [NNX10AI77G]
  5. NSF [ATM0960594]
  6. NASA [NNX10AI77G, 132119, 145933, NNX11AG76G, NNX11AH16G, 144307] Funding Source: Federal RePORTER
  7. Div Of Chem, Bioeng, Env, & Transp Sys
  8. Directorate For Engineering [0960256] Funding Source: National Science Foundation

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We report data on the martian meteorite Northwest Africa (NWA) 7034, which shares some petrologic and geochemical characteristics with known martian meteorites of the SNC (i.e., shergottite, nakhlite, and chassignite) group, but also has some unique characteristics that would exclude it from that group. NWA 7034 is a geochemically enriched crustal rock compositionally similar to basalts and average martian crust measured by recent Rover and Orbiter missions. It formed 2.089 +/- 0.081 billion years ago, during the early Amazonian epoch in Mars' geologic history. NWA 7034 has an order of magnitude more indigenous water than most SNC meteorites, with up to 6000 parts per million extraterrestrial H2O released during stepped heating. It also has bulk oxygen isotope values of Delta O-17 = 0.58 +/- 0.05 per mil and a heat-released water oxygen isotope average value of Delta O-17 = 0.330 +/- 0.011 per mil, suggesting the existence of multiple oxygen reservoirs on Mars.

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