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