Chronology of martian breccia NWA 7034 and the formation of the martian crustal dichotomy
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- William S. Cassata
- Nuclear and Chemical Sciences Division, Lawrence Livermore National Laboratory, Livermore, CA 94550, USA.
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- Benjamin E. Cohen
- Isotope Geoscience Unit, Scottish Universities Environmental Research Centre, Rankine Avenue, East Kilbride, G75 0QF, UK.
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- Darren F. Mark
- Isotope Geoscience Unit, Scottish Universities Environmental Research Centre, Rankine Avenue, East Kilbride, G75 0QF, UK.
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- Reto Trappitsch
- Nuclear and Chemical Sciences Division, Lawrence Livermore National Laboratory, Livermore, CA 94550, USA.
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- Carolyn A. Crow
- Nuclear and Chemical Sciences Division, Lawrence Livermore National Laboratory, Livermore, CA 94550, USA.
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- Joshua Wimpenny
- Nuclear and Chemical Sciences Division, Lawrence Livermore National Laboratory, Livermore, CA 94550, USA.
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- Martin R. Lee
- School of Geographical and Earth Sciences, University of Glasgow, G12 8QQ, UK.
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- Caroline L. Smith
- School of Geographical and Earth Sciences, University of Glasgow, G12 8QQ, UK.
書誌事項
- 公開日
- 2018-05-04
- DOI
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- 10.1126/sciadv.aap8306
- 公開者
- American Association for the Advancement of Science (AAAS)
説明
<jats:p>The metamorphic history of martian meteorite NWA 7034 suggests that the martian crustal dichotomy may have formed within 100 million years of planetary formation.</jats:p>
収録刊行物
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- Science Advances
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Science Advances 4 (5), eaap8306-, 2018-05-04
American Association for the Advancement of Science (AAAS)
