Arabian Journal of Geosciences

, Volume 8, Issue 10, pp 7973–7991 | Cite as

Sedimentological characteristics of continental sabkha, south Western Desert, Egypt

Original Paper
  • 178 Downloads

Abstract

Continental sabkha is recorded in the extreme middle part of the south Western Desert of Egypt representing one of the most promising areas for sustainable development, especially for agriculture. The geomorphologic units of the area are formed under the influence of structural, lithological, and/or climatic controls. These units include pediplain, depressions, mass-wasted blocks, residual hills, drainage lines, and aeolian landforms. The effective deflation process is reinforced by the lack of protective vegetation cover and the susceptibility of weakly consolidated rocks to wind removal. Different rock units covering the area range in age from Early Cretaceous to Quaternary. Quaternary deposits include playa/sabkha deposits where the continental sabkha is divided into four zones A, B, C, and D. Underground waters coming from the north and east were progressively enriched in solute by interaction with the surrounding sedimentary and igneous rocks. Most of the evaporite minerals grow displacively as a result of evaporative pumping. Mineralogically, the continental sabkha salt complex includes gypsum, natroalunite, tamarugite, bloedite, eugsterite, nitratine, halite, and D’ansite. Some of the major and trace elements (SiO2, Al2O3, Fe2O3, MgO, CaO, Na2O, K2O, as well as Rb, Ba, Zr, Sr, Y, V, and Zn) were measured. The correlation and enrichment of these major and trace elements indicate the origin of the salt complex in the sabkha.

Keywords

Continental sabkha Evaporites Sedimentology Geochemistry 

Notes

Acknowledgments

The authors would like to express their grateful to all the stuff members and employee of Nuclear Materials Authority (NMA) of Egypt for kind assistance and great help during the progress of this work.

References

  1. Abu Al-Izz MS (1971) Landforms of Egypt. Amer Univ, Cairo press, p 281Google Scholar
  2. Afifi NM (2001) Geology and uranium potentiality of radioactive anomalies in Nusab El-Balgoum area, Western Desert, Egypt. M Sc thesis, FacSci, El Mansoura Univ, Egypt, p 170Google Scholar
  3. Albritton CC, Brooks JE, Issawi B, Swedan A (1990) Origin of the Qattara depression, Egypt. Geol Soc Amer Bull 102:952–960CrossRefGoogle Scholar
  4. Barthel KW, Boettcher R (1978) Abu Ballas formation: a significant lithostratigrahpic unit of the former “Nubian Series”. Mitt Bayer Staats Palaontol Hist Geol 18:153–166Google Scholar
  5. El Deftar T (ed) (1988) Internal report on south Western Desert. Geol Surv Auth, Egypt, p 29Google Scholar
  6. Fitzpatrick R, Paul Shand P, Raven M, McClure S (2010) Occurrence and environmental significance of sideronatrite and other mineral precipitates in Acid Sulfate Soils. 19th World Cong Soil Sci, Soil Solutions for a Changing World, Brisbane, Australia, 80–83Google Scholar
  7. Glennie KW (1970) Desert sedimentary environments. Developments in Sedimentology, 14, El Sevier Publ Co, p 222Google Scholar
  8. Haynes CV (1980) Geological evidence of pluvial climates in the Nabta area of the Western Desert, Egypt. In: Wendrof F, Schild R (eds) Prehistory of the Eastern Sahara. Academic, New York, pp p. 353–p. 371Google Scholar
  9. Haynes CV (1982) Great sand sea and Selima sand sheet, Eastern Sahara: geochronology and desertification. Science 217:627–633CrossRefGoogle Scholar
  10. Henning D, Flohn H (1977) Climate aridity index map. MN Conf Desertification, Nairobi, UNEP, UN Foc AlConf74/31Google Scholar
  11. Hussein HK (2002) Geology and radioactivity of Bir Abu El Hussein area, south Western Desert, Egypt. MSc thesis, Geol Dept, Fac Sci, Cairo Univ, Egypt, p 87Google Scholar
  12. Issawi B (1971) Geology of Darb El Arbain, Western Desert. Annals Geol Surv Egypt 1:53–92Google Scholar
  13. Kehl H, Bornkamm R (1993) Landscape ecology and vegetation units of the Western Desert of Egypt. Catena Supp 26:155–178Google Scholar
  14. Klitzsch E (1984) Northwestern Sudan and bordering areas: geological development since Cambrian time. Berliner Geowiss Abh A 50:23–45Google Scholar
  15. Klitzsch E, Lejal-Nicol A (1984) Flora and fauna from strata in southern Egypt and northern Sudan. Berlin Geowissenschaft Abhand Lungen A 50:47–79Google Scholar
  16. Kröpelin S (1993) Geomorphology, landscape evolution and paleo-climates of south West Desert, Egypt. In: Meissner B, Wycisk P (eds) Geopotential and ecology (analysis of a desert region), Catena Supplement 26, p 199Google Scholar
  17. Norrish K, Chappell BW (1966) X-ray fluorescence spectrography. In: Zussman J (ed) Physical methods of determinative mineralogy. Academic, New York, pp 161–214Google Scholar
  18. Said R (1962) The geology of Egypt. Elsevier, p 377Google Scholar
  19. Said R (1983) Remarks on the origin of the landscape of the Eastern Sahara. J Afr Earth Sci 1:153–158Google Scholar
  20. Shapiro L, Brannock WW (1962) Rapid analysis of silicates, carbonates and phosphate rocks. US Geol Surv Bull :1144-A, p 56Google Scholar
  21. Topper RPM, Lugli S, Manzi V, Roveri M, Meijer PT (2014) Precessional control of Sr ratios in marginal basins during the Messinian Salinity Crisis? Geochem Geophys Geosys. doi:10.1002/2013GC005192 Google Scholar
  22. Vergouwen L (1981) Eugsterite, a new salt mineral. Amer Mineralog 66:632–636Google Scholar
  23. Walther J (1912) Das gesetz der wüstenbildung in Gegenwart und Vorzeit. Quele and Meyer, Leipzig, 342 pGoogle Scholar

Copyright information

© Saudi Society for Geosciences 2015

Authors and Affiliations

  1. 1.Department of Geology and Geophysics, College of ScienceKing Saud UniversityRiyadhSaudi Arabia
  2. 2.Department of Geology, Faculty of ScienceCairo UniversityGizaEgypt
  3. 3.Egyptian Nuclear Materials Authority (ENMA)CairoEgypt

Personalised recommendations