geologic units in gusev crater - nasa · 2003. 7. 14. · gusev crater stratigraphy • duricrust...
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![Page 1: Geologic Units In Gusev Crater - NASA · 2003. 7. 14. · GUSEV CRATER STRATIGRAPHY • Duricrust or cap layer in low-inertia material; composed of or mantled by fine sediments •](https://reader036.vdocument.in/reader036/viewer/2022062510/611786472a3f5206c2418391/html5/thumbnails/1.jpg)
Geologic Units In Gusev Crater
Ross Irwin
Center for Earth and Planetary StudiesNational Air and Space Museum
Smithsonian Institution
4th MER Landing Site Workshop January 9, 2003
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Daytime IR contrasts
• Dust devil tracks• Gardened crater floor• Ejecta of larger craters• Etched areas
THEMIS I00881002 32 km across
MD
IM/D
aytim
e TH
EMIS
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MOC E17-00827, 3.76 km across
High-inertia material exposed in etched terrain
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GUSEV CRATER STRATIGRAPHY• Duricrust or cap layer in low-inertia material; composed of or mantled by fine sediments
• Low-inertia layer, gardened and etched
• High-inertia layer(s) in ejecta and etched terrain
• ~1 km Ma’adim deposit beneath surface layers
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CONTRASTS BETWEEN COARSE AND FINE LAYERS
18 km acrossTHEMIS IR I00856001
32 km across
MOC E02-00665 and E03-01511, 5.8 km across
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Etched terrain IR contrasts are due to material differences, not illumination
18 km acrossTHEMIS IR I00856001
32 km across
THEMIS night IR I01149002, 17 km across
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DURICRUST OR CAP LAYER
• Crater fill preserved as positive relief
• Sharp transition to gardened plains
• Isolated mesas
• Some elongation but L:W of knobs < 4:1
MOC E05-00471, 3 km across
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IMPACT GARDENING
MOC NA E18-00950
3.5 km acrossMDIM/Daytime THEMIS
100m contour
Fill of interior craters has lower populations
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DUST DEVIL TRACKS
MOC E10-02768 3 km across
MOC E15-00362 3 km across
MDIM/Daytime THEMIS
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TESTABLE HYPOTHESES: Coarse layer Exposure within the landing ellipse is limited; most common exposures are in crater ejecta
• Composition, size, sorting, rounding? Could be fluvial deposit from Ma’adim, intracrater fluvial deposit, duricrust, or volcanic material. Magnetic?
Use imagers, APXS, Mini-TES
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TESTABLE HYPOTHESES: Fine layer
Extensive within the landing ellipse & ejecta of small craters
• Composition, size, sorting, rounding? Scale of layering? Crossbeds? Vertical sorting? Could be varves, pyroclastic, other airfall
• Use imagers, APXS, Mini-TES
MOC E17-00827,
3.76 km across
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TESTABLE HYPOTHESES: Duricrust (?) and dust devils
Presumably extensive within the landing ellipse
• Are dust devils transporting a lag material? If so, what is its composition, size, etc.? What material is being exposed in the tracks?
• What cement is responsible for crust (if any)? Strength properties (RAT): how well cemented?
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TESTABLE HYPOTHESES: Weathering
• Studies of weathering on Mars have remained largely theoretical. If fluvial or lacustrine deposits are identified, are they chemically altered or the products of physical weathering and rapid transport? This has implications for paleoclimate. Is active physical or chemical weathering observed?
• Use Mini-TES, APXS, and Mossbauer for sediment composition information
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ANALOG STUDIESDichotomy boundary sediments
MOC E10-02784 3 km across
THEMIS I00957001 32 km across
MOC E05-01183 3 km across