Small edifice features in Chryse Planitia, Mars: Assessment of a mud volcano hypothesis
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Small edifice features up a few km in diameter widely occur in Chryse Planitia, Mars.

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Their overall diverse morphology is consistent with the mud volcano origin.

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Their detailed characteristics may require conditions unique to martian environment.

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Our CRISM analysis has detected nanophase ferric minerals and hydrated minerals.

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Mud volcanism may have been promoted by rapid sedimentation in Chryse Planitia.

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