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Magnetite whiskers and platelets in the ALH84001 Martian meteorite: Evidence of vapor phase growth
Abstract
Nanometer-sized magnetite crystals associated with carbonates in fracture zones within Martian meteorite ALH84001 have been examined using analytical transmission electron microscopy. Some of the crystals exhibit distinctive morphologies: filamentary rods and ribbon, and platelets. The rods and ribbons are elongated along the crystallographic [100] and [111] directions. Some of the rods contain microstructural defects indicating that they grew by spiral growth about screw dislocations. Platelets are flattened along the [100] and [110] directions. These unique morphologies and microstructures constrain the growth conditions of magnetite. The whiskers and platelets most likely formed in the temperature range 500-800 degrees C by direct condensation from a vapor or precipitation from a supercritical fluid, and their properties are inconsistent with a biogenic origin.
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Search for Past Life on Mars: Possible Relic Biogenic Activity in Martian Meteorite ALH84001
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Chicot, D., Mendoza, J., Zaoui, A., Louis, G., Lepingle, V., Roudet, F., & Lesage, J. (2011) · Materials Chemistry and Physics · doi:10.1016/j.matchemphys.2011.05.056 · Cited by 238
Domagal-Goldman, S. D., Wright, K. E., Domagal-Goldman, S. D., Wright, K. E., Adamala, K., Arina de la Rubia, L., Bond, J., Dartnell, L. R., Goldman, A. D., Lynch, K., et al. (2016) · Astrobiology · doi:10.1089/ast.2015.1460 · Cited by 136
“As a result, we now know that abiological processes could have created these signals, and the meteorite is not therefore widely considered proof of life beyond Earth (Bradley et al., 1996, 1997; Frankel and Buseck, 2000; Buseck et al., 2001; McKay et al., 2003; Treiman, 2003).”
CORRIGAN, C. M., & HARVEY, R. P. (2004) · Meteoritics & Planetary Science · doi:10.1111/j.1945-5100.2004.tb00047.x · Cited by 50
Self-citation
Metadata
- Authors
- Bradley, J. P., Harvey, R. P., & McSween, H. Y.
- Affiliations
- Georgia Institute of Technology (US)
- Case Western Reserve University (US)
- University of Tennessee at Knoxville (US)
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 1996-12
- Volume
- 60
- Issue
- 24
- Pages
- 5149-5155
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W2081654683
- Cited by
- 105
- References
- 1
- Citations by year
- 2025: 1 · 2024: 2 · 2023: 1 · 2022: 1 · 2021: 1 · 2020: 4 · 2018: 3 · 2016: 2 · 2015: 2 · 2014: 4 · 2013: 1 · 2012: 2
- FWCI
- 11.82
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geochimica et Cosmochimica Acta (publishedVersion)
- PubMed (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Planetary Science and Exploration
- Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Astro and Planetary Science
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geomagnetism and Paleomagnetism Studies
- Keywords
- ALH84001, Martian meteorites, vapor growth, crystal morphology, spiral growth, screw dislocations, microstructural defects, fracture zones, carbonates, biogenic origin
- MeSH terms
- Carbonates, Hot Temperature, Iron, Microscopy, Electron, Oxides, Earth, Planet, Mars, Meteoroids, Ferrosoferric Oxide
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