Evidence for Persistent Flow and Aqueous Sedimentation on Early Mars

Author:

Malin Michael C.1,Edgett Kenneth S.1

Affiliation:

1. Malin Space Science Systems, Post Office Box 910148, San Diego, CA 92191, USA.

Abstract

Landforms representative of sedimentary processes and environments that occurred early in martian history have been recognized in Mars Global Surveyor Mars Orbiter Camera and Mars Odyssey Thermal Emission Imaging System images. Evidence of distributary, channelized flow (in particular, flow that lasted long enough to foster meandering) and the resulting deposition of a fan-shaped apron of debris indicate persistent flow conditions and formation of at least some large intracrater layered sedimentary sequences within fluvial, and potentially lacustrine, environments.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference36 articles.

1. The debate over whether liquid water or some other fluid (including gas-fluidized dry flow) is responsible for erosional landforms on Mars (which include but are not limited to the martian outflow channels valley networks and gullies) is not specifically addressed in this work. Most geoscientists familiar with martian landforms agree that water is the most likely candidate fluid.

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