Age and Stratigraphic Relationships in Massif-Debris-Apron Terrain in Western Phlegra Montes, Mars

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Scientific paper

SHARAD returns from lobate debris aprons (LDA) near Phlegra Montes may
show similarly high ice contents to other LDA on Mars; geomorphology and
surface ages of the deposits confirm this detection and support a
debris-covered-glacier origin for LDA.

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