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• W1983027048 endingPage "1937" @default.
• W1983027048 startingPage "1927" @default.
• W1983027048 abstract "Layered and massive outcrops on Mars, some as thick as 4 kilometers, display the geomorphic attributes and stratigraphic relations of sedimentary rock. Repeated beds in some locations imply a dynamic depositional environment during early martian history. Subaerial (such as eolian, impact, and volcaniclastic) and subaqueous processes may have contributed to the formation of the layers. Affinity for impact craters suggests dominance of lacustrine deposition; alternatively, the materials were deposited in a dry, subaerial setting in which atmospheric density, and variations thereof mimic a subaqueous depositional environment. The source regions and transport paths for the materials are not preserved." @default.
• W1983027048 created "2016-06-24" @default.
• W1983027048 creator A5014235466 @default.
• W1983027048 creator A5059880500 @default.
• W1983027048 date "2000-12-08" @default.
• W1983027048 modified "2023-10-09" @default.
• W1983027048 title "Sedimentary Rocks of Early Mars" @default.
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• W1983027048 doi "https://doi.org/10.1126/science.290.5498.1927" @default.
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