Abstract
NanoSIMS measurements record δD values up to +4725‰ in
Lafayette which reveal martian waters of crustal origin are incorporated
into the smectite and adjacent olivine.
Original language | English |
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Article number | 5101 |
Number of pages | 1 |
Journal | Meteoritics and Planetary Science |
Volume | 48 |
Issue number | s1 |
Early online date | 1 Jul 2013 |
DOIs | |
Publication status | Published - Jul 2013 |