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Title: Hydrous olivine alteration on Mars and Earth

Journal Article · · Meteoritics and Planetary Science
DOI:https://doi.org/10.1111/maps.13479· OSTI ID:1644102

Abstract Hydrous alteration of olivine macrocrysts in a Martian olivine phyric basalt, NWA 10416, and a terrestrial basalt from southern Colorado are examined using SEM, EPMA, TEM, and µXRD techniques. The olivines in the meteorite contain linear nanotubes of hydrous material, amorphous areas, and fluid dissolution textures quite distinct from alteration identified in other Martian meteorites. Instead, they bear resemblance to terrestrial deuteric alteration features. The presence of the hydrous alteration phase Mg‐laihunite within the olivines has been confirmed by µXRD analysis. The cores of the olivines in both Martian and terrestrial samples are overgrown by unaltered rims whose compositions match those of a separate population of groundmass olivines, suggesting that the core olivines are xenocrysts whose alteration preceded crystallization of the groundmass. The terrestrial sample is linked to deep crustal metasomatism and the “ignimbrite flare‐up” of the Oligocene epoch. The comparison of the two samples suggests the existence of an analogous relatively water‐rich magmatic reservoir on Mars.

Research Organization:
Argonne National Laboratory (ANL), Argonne, IL (United States)
Sponsoring Organization:
USDOE Office of Science (SC), Basic Energy Sciences (BES). Chemical Sciences, Geosciences & Biosciences Division (CSGB); National Aeronautics and Space Administration (NASA); National Science Foundation (NSF); New Mexico Space Grant Consortium; USDOE
Grant/Contract Number:
FG02-94ER14466; AC02-06CH11357; EAR-1634415
OSTI ID:
1644102
Alternate ID(s):
OSTI ID: 1630363
Journal Information:
Meteoritics and Planetary Science, Vol. 55, Issue 5; ISSN 1086-9379
Publisher:
WileyCopyright Statement
Country of Publication:
United States
Language:
ENGLISH
Citation Metrics:
Cited by: 7 works
Citation information provided by
Web of Science

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