Arkenu structures
| Arkenu structures | |
|---|---|
NASA World Wind | |
| Impact crater/structure | |
| Diameter | 10 kilometres (6.2 mi) and 6.8 kilometres (4.2 mi) |
| Age | <120 Ma |
| Exposed | Yes |
| Drilled | No |
| Location | |
| Country | Libya |
| Municipality | Jabal Arkanu |
  | |
The Arkenu structures, also known as the Arkenu craters, are a pair of prominent circular geological structures in eastern Libya. The structures are approximately 10 kilometres (6.2 mi) and 6.8 kilometres (4.2 mi) in diameter, and lie about 70 kilometres (43 mi) west of Jabal Arkanu on the eastern margin of the al-Kufrah Basin.[1][2]
It has been argued that both structures were formed by simultaneous
meteorite impacts. Field investigations by Dr. P. Paillou, Dr. A. Rosenqvist, and others reported the presence of impact breccias at the structures’ bottoms, shatter cones pointing toward the center of the structures, and microscopic planar deformation features (PDFs) found in quartz grains of sandstones outcropping in the structures. Based on these reports and other observations, it was proposed that both structures are extraterrestrial impact craters that were formed simultaneously as a double impact event less than 140 million years ago (Jurassic or younger).[1]
More recently, on the basis of field,
monchiquites) directly associated with each circular feature. Based on these and other observations, it was concluded that the Arkenu structures are stocks of porphyritic syenitic that have intruded the Nubia Formation to form rather simple and eroded ring dike complexes. Hydrothermal activity that followed the intrusion of these ring dike complexes resulted in the formation of massive magnetite–hematite deposits and dikes of silicified sandstone.[2][3] As a result of this research, the Arkenu structures were removed from and are currently not listed in the Earth Impact Database.[4]
References
- ^ a b Paillou P., A. Rosenqvist A., J.M. Malezieux, B. Reynard, T. Farr, and E. Heggy (2003) Discovery of a double impact crater in Libya: The astrobleme of Arkenu. Comptes Rendus Geoscience. vol. 335, no. 15, pp. 1059–1069.
- ^ a b Cigolini, C, C Laiolo, and M Rossetti (2012) Endogenous and nonimpact origin of the Arkenu circular structures (al-Kufrah basin-SE Libya) Meteoritics & Planetary Science. 47(11):1772–1788.
- ^ Di Martino, M, C Cigolini, and L. Orti (2008) Non-impact origin of the Arkenu craters (Libya) Large Meteorite Impacts and Planetary Evolution IV, 17–21 August, Vredefort Dome South Africa. abstract no. 3012, Lunar and Planetary Institute, Houston, Texas.
- ^ Anonymous (nd) Africa (Impact Craters) Archived 2015-12-22 at the Wayback Machine, Earth Impact Database Archived 2015-02-07 at the Wayback Machine, Planetary and Space Science Centre, University of New Brunswick, New Brunswick, Canada.
External links
- Brügge, N. (2012) Remarks to the origin of the craters around Gilf Kebir and Djebel Uweinat (Egypt)and the supposed impact craters of Libya, Sahara Trekking.
- Di Martino, M. (2010) Impact and non-impact craters in eastern Sahara INAF – Osservatorio Astronomico di Torino Talk of the "International Workshop on Paolo Farinella (1953-2000): the Scientists, the man", Pisa, 14–16 June 2010
- Willis, K. J. (2008) Arkenu Craters, Libya : Image of the Day. Earth Observatory, EOS Project Science Office, NASA Goddard Space Flight Center, Greenbelt, Maryland.
22°6′5″N 23°47′54″E / 22.10139°N 23.79833°E
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