Relief Inversion at the Deuteronilus Contact of the Isidis Basin, Mars: Implications for the Formation of the Isidis Interior Plains

Details Relief Inversion at the Deuteronilus Contact of the Isidis Basin, Mars: Implications for the Formation of the Isidis Interior Plains Relief Inversion at the Deuteronilus Contact of the Isidis Basin, Mars: Implications for the Formation of the Isidis Interior Plains

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.2016e&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.2016

Physics

Scientific paper

Valleys that occur on the Isidis exterior plains continue across the
Deuteronilus contact and occur then as ridges. We propose a
fluvio-glacial scenario for the formation of relief inversion at the
Deuteronilus contact.

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