Abstract
Using satellite imagery, we detected more than 1300 small crater-like structures distributed over an area of 40,000 km2 in the Western Egyptian Desert, close to the Gilf Kebir plateau. Sixty-two of them were visited in the field, and morphological observations, rock samples and ground-penetrating radar data were obtained. After presenting our fieldwork results, we discuss two hypotheses for their origin: hydrothermal vent complexes and meteorite impacts. At present, none of them fully satisfies the available observations.
| Original language | English |
|---|---|
| Pages (from-to) | 281-299 |
| Number of pages | 19 |
| Journal | Journal of African Earth Sciences |
| Volume | 46 |
| Issue number | 3 |
| DOIs | |
| Publication status | Published - Oct 2006 |
| Externally published | Yes |
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