Noble gases in 18 Martian meteorites and angrite Northwest Africa 7812—Exposure ages, trapped gases, and a re‐evaluation of the evidence for solar cosmic ray‐produced neon in shergottites and other achondrites

Author:

Wieler R.1,Huber L.1,Busemann H.1,Seiler S.1,Leya I.2,Maden C.1,Masarik J.3,Meier M. M. M.1,Nagao K.4,Trappitsch R.5,Irving A. J.6

Affiliation:

1. Department of Earth Sciences ETH Zürich NW C84 CH8092 Zürich Switzerland

2. Space Research and Planetary Sciences University of Bern CH‐3001 Bern Switzerland

3. Department of Nuclear Physics & Biophysics Comenius University SK‐84248 Bratislava Slovakia

4. Geochemical Research Center Graduate School of Science University of Tokyo 7‐3‐1 Hongo Bunkyo‐ku Tokyo 113‐0033 Japan

5. Department of the Geophysical Sciences and Chicago Center for Cosmochemistry The University of Chicago Chicago Illinois 60637 USA

6. Department of Earth & Space Sciences University of Washington Seattle Washington 98195 USA

Funder

Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Reference110 articles.

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

2. AndreasenR. RighterM. LapenT. J. IrvingA. J. NishiizumiK. JullA. J. T. andCaffeeM.2014.Lead‐lead isotope systematics and terrestrial and ejection ages of early Amazonian depleted shergottite Northwest Africa 7635(abstract #2865). 45th Lunar and Planetary Science Conference. CD‐ROM.

3. BegemannF.andSchultzL.1988.The influence of bulk chemical composition on the production rate of cosmogenic nuclides in meteorites. Proceedings 19th Lunar and Planetary Science Conference. pp.51–52.

4. Spallation production of 3He, 21Ne, and 38Ar from target elements in the Bruderheim chondrite

5. Relative abundances of argon, krypton, and xenon in the Martian atmosphere as measured in Martian meteorites

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