A new approach to cosmogenic corrections in 40Ar/39Ar chronometry: Implications for the ages of Martian meteorites

Author:

Cassata W.S.,Borg L.E.

Funder

U.S. Department of Energy by Lawrence Livermore National Laboratory

NASA Cosmochemistry program

NASA Mars Fundamental Research Program

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference50 articles.

1. Halogen content and Cl isotope systematics on Mars: from the atmosphere to the hydrosphere to the lithosphere;Bellucci,2016

2. Al-26, Be-10, and Mn-53 in Martian meteorites;Berezhnoy,2010

3. 40Ar/39Ar ages and trapped argon in Martian shergottites, Chassigny, and Allan Hills 84001;Bogard;Meteorit. Planet. Sci.,1999

4. 39Ar–40Ar dating of the Zagami Martian shergottite and implications for magma origin of excess 40Ar;Bogard;Meteorit. Planet. Sci.,2008

5. Martian volatiles: isotopic composition, origin, and evolution;Bogard;Space Sci. Rev.,2001

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1. The complexities in interpreting Argon isotopes;Methods and Applications of Geochronology;2024

2. Formation and interior evolution of Mars;Reference Module in Earth Systems and Environmental Sciences;2024

3. Synchronising rock clocks of Mars' history: Resolving the shergottite 40Ar/39Ar age paradox;Earth and Planetary Science Letters;2023-11

4. A window into atmospheric escape on early Mars provided by argon isotopes in a Martian meteorite;Geochimica et Cosmochimica Acta;2022-07

5. 40 Ar/ 39 Ar ages of Northwest Africa 7034 and Northwest Africa 7533;Meteoritics & Planetary Science;2021-03

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