Probing structural elements of small buried craters using ground-penetrating radar in the southwestern Egyptian desert

Implications for Mars shallow sounding

Essam Heggy, Philippe Paillou

Research output: Contribution to journalArticle

9 Citations (Scopus)

Abstract

We report results from a field survey performed on a recently discovered impact field in the southwestern Egyptian desert, using a 270 MHz Ground-Penetrating Radar (GPR). This hyperarid region has significant similarities to the Martian heavily eroded mid-latitude cratered terrains in terms of crater density, size, and geomorphology. Profiles across small-buried craters revealed a coherent sequence of tilted layers constituting the cratonic infill resulting from aeolian deposits. In the intercrater areas the radargram revealed a poorly-defined subsurface stratigraphy and the presence of shallow structural elements associated with potential evidences of the consequences of the shock effects, i.e., faulting, fractures, and chaotic bedrock. The radar-penetration depth varied from 2 to 15 m, depending mainly on the amplitude of the volume and multiple scattering in the subsurface, caused by fractures and debris created by the impacts. We conclude that mid-frequency GPR onboard future Martian rovers can successfully perform similar structural mapping.

Original languageEnglish
Article numberL05202
JournalGeophysical Research Letters
Volume33
Issue number5
DOIs
Publication statusPublished - 16 Mar 2006
Externally publishedYes

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ground penetrating radar
deserts
sounding
craters
mars
crater
Mars
desert
geomorphology
eolian deposit
stratigraphy
bedrock
infill
debris
field survey
radar
faulting
penetration
shock
deposits

ASJC Scopus subject areas

  • Earth and Planetary Sciences (miscellaneous)

Cite this

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