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Hesperian equatorial thermokarst lakes in Ares Vallis as evidence for transient warm conditions on Mars (2010)

First Author: Warner N

Attributed to: Origin and evolution of the outflow channels on Mars using HRSC 3-D imaging funded by STFC

Abstract

No abstract provided

Bibliographic Information

Digital Object Identifier: http://dx.doi.org/10.1130/g30579.1

Publication URI: http://dx.doi.org/10.1130/g30579.1

Type: Journal Article/Review

Parent Publication: Geology

Issue: 1