| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 1774922 | Icarus | 2008 | 7 Pages |
Abstract
Polygonal crack systems with domal microrelief imaged by the Mars Exploration Rover (MER) Opportunity show remarkable similarity to terrestrial crack systems developed on outcrop surfaces. Study of Jurassic Navajo Sandstone surfaces show development of crack systems in relatively isotropic host rock as a result of tensile weathering stresses. These terrestrial analogs are utilized to understand potential weathering processes on Mars.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Space and Planetary Science
Authors
Marjorie A. Chan, W. Adolph Yonkee, Dennis I. Netoff, Winston M. Seiler, Richard L. Ford,