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Dating the Martian meteorite Zagami by the (87)Rb-(87)Sr isochron method with a prototype in situ resonance ionization mass spectrometer

RATIONALE: The geologic history of the Solar System builds on an extensive record of impact flux models, crater counts, and ∼270 kg of lunar samples analyzed in terrestrial laboratories. However, estimates of impactor flux may be biased by the fact that most of the dated Apollo samples were only ten...

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Detalles Bibliográficos
Autores principales: Scott Anderson, F, Levine, Jonathan, Whitaker, Tom J
Formato: Online Artículo Texto
Lenguaje:English
Publicado: BlackWell Publishing Ltd 2015
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4297357/
https://www.ncbi.nlm.nih.gov/pubmed/25641494
http://dx.doi.org/10.1002/rcm.7095