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Mawrth Candidate Landing Site (Dawn Sumner, July 27, 2010)

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Presentation on theme: "Mawrth Candidate Landing Site (Dawn Sumner, July 27, 2010)"— Presentation transcript:

1 Mawrth Candidate Landing Site (Dawn Sumner, July 27, 2010)
Site Context Mineral Stratigraphy Models for Clay Mineral Accumulation Implications for Biosignature Formation & Preservation

2 Mawrth Site is in Far Western Arabia Terra
Approximate outline of “Arabia Terra” is shown. Interpretation of exact “boundaries” may vary depending on who you ask.

3 Oyama Crater & Mawrth Vallis

4 Landing Ellipse Oyama Crater

5 Michalski et al. 2010

6 Loizeau et al. 2010 Blue ~ Al-clay mineral detections
Orange ~ Fe, Mg-clay mineral detections Loizeau et al. 2010

7 Models for Clay Minerals (not mutually exclusive)
Alteration of Bedrock (igneous or other) “Soils”, hydrothermal, or water table Alteration as Rock Accumulated Many “soils” Alteration of hydrous pyroclasitcs Alteration associated with impacts Sedimentary Accumulation of Clay Minerals Fluvial, lacustrine, unknown

8 Bedrock Alteration Michalski & Noe Dobrea, 2007
Issues: Variable Alteration/Mineralogy Depth of Alteration Extent of Chemical Leaching Origin of Bedrock

9 Alteration During Accumulation
Issues: Consistency of Mineral Stratigraphy Variations in Mineralogy with Depth Pervasiveness of Alteration Sumner, in prep.

10 (no published images of models to my knowledge)
Deposition of Clays Issues: No Reported Sedimentary Geometries No Basin Margins to Confine Flow Only Rare Channels, Post Deposition of Light Toned Units Compositionally Defined Layers “Drape” Topography (no published images of models to my knowledge)

11 Biosignature Formation and Preservation (Summons et al., in review)


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