Gweni-Fada Crater
   HOME

TheInfoList



OR:

Gweni-Fada is a
meteorite A meteorite is a solid piece of debris from an object, such as a comet, asteroid, or meteoroid, that originates in outer space and survives its passage through the atmosphere to reach the surface of a planet or Natural satellite, moon. When the ...
crater Crater may refer to: Landforms *Impact crater, a depression caused by two celestial bodies impacting each other, such as a meteorite hitting a planet *Explosion crater, a hole formed in the ground produced by an explosion near or below the surfac ...
in the Ennedi Plateau, Chad.VINCENT P.M., BEAUVILAIN A.
The circular structure of Gweni-Fada, Ennedi : a new meteoritic impact crater in northern Chad
C.R. Acad. Sci. Paris, t. 323, série II a, pp. 987-997, 1996.
The Gweni Fada structure was first noted on the map NE 34 X Fada of the IGN (National Geographic Institute France) and aerial photographs in the 1950s of IGN by
Alain Beauvilain Alain may refer to: People * Alain (given name), common given name, including list of persons and fictional characters with the name * Alain (surname) * "Alain", a pseudonym for cartoonist Daniel Brustlein * Alain, a standard author abbreviatio ...
(Paris X- Nanterre University). In April 1995, at the initiative of CNAR (National Center to Help Research of Chad) a team of French geologists (Pierre Vincent, University of Clermont-Ferrand, Alain and Najia Beauvilain, CNAR Chad) visited the site and reported evidence of shock metamorphism within rock samples they had collected inside the structure. Centered at 17°25′N and 21°45′E, being slightly wider in the NW-SE direction (cf. topographic map), the asymmetric structure is deeply eroded. A broad depression (ø 12 km) forms a crescent around two thirds of the inner complex zone. On the northern side, an elevated outer ring of outward-dipping sandstones surrounds the depression. In its south, the external depression is absent. The inner zone (ø 10 km) consists of a rugged terrain with hills several hundred meters in height. The latter may be remnants of the central uplift (see topographic map). The age is estimated to be less than 345 million years (
Carboniferous The Carboniferous ( ) is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago ( Mya), to the beginning of the Permian Period, million years ago. The name ''Carbonifero ...
). It is older than that of Aorounga because its coverage of impactite has disappeared as a result of erosion.


See also

*
List of impact craters in Africa __TOC__ Confirmed impact craters This list of impact craters in Africa includes all 20 confirmed impact craters as listed in the Earth Impact Database. These features were caused by the collision of large meteorites or comets with the Ea ...
** Aorounga crater


References


Further reading

* Becq-Giraudon, J. -F., Rouzeau, O., Goachet, E. and Solages, S.
Meteoritic impact origin of the annular depression of Aorounga, Chad (Africa)
C. R. Acad. Sci. Paris, t. 315, série II, p. 83-88. 1992. * Koeberl, C., African meteorite impact craters: Characteristics and geological importance. Journal of African Earth Sciences, v. 18, pp. 263–295. 1994. * Koeberl, C., Reimold, W. U., Cooper, G., Cowan, D. and Vincent, P. M.
Aorounga and Gweni Fada impact structures, Chad: Remote sensing, petrography, and geochemistry of target rocks
Meteoritics & Planetary Science, 40, No 9/10 P. 1455 - 1471. 2005. * Koeberl, C., Reimold, W.U., Vincent, P. M., Brandt, D.
Aorounga and Gweni Fada Impact Structures, Chad, Central Africa : Petrology and Geochemistry of Target Rocks
LPSC XXIX, Lunar and Planetary Institute, Houston, TX, (CD-ROM). 1998. * McHone J.F., Greeley, R., More impact and impact-like structures on the SIR-C radar; Europe, Africa, and Arabian Peninsula (abstract). Lunar and Planetary Science XXVIII, pp. 915–916. 1997. * Miallier, D., Sanzelle, S., Falgueres, C., Fain, J., Pilleyre, Th. And Vincent, P.M., TL and ESR of quartz from the astrobleme of Aorounga (Sahara of Chad), Quaternary Science Reviews, Vol 16 (3-5), pp. 265–274. 1997. * Ocampo, A. C., Pope, K. O., Shuttle Imaging Radar (SIR-C) Images Reveal Multiple Impact Craters at Aorounga, Northern Chad, 27th Lunar and Planetary Science Conference. 1996. * Vincent, P. M., Beauvilain, A., Boudeulle, M. and Moutaye, A.H., The astrobleme of Aorounga (Sahara of Tchad): Preliminary structural data (abstract). European Science Foundation, Third International Workshop. Shock Wave Behaviour of Solids in Nature and Experiments, Limoges, France. 1994.


External links


Description and exclusive pictures of Gweni-Fada crater in the field by Alain Beauvilain
{{Impact cratering on Earth Impact craters of Chad Carboniferous impact craters Carboniferous Africa Ennedi-Ouest Region