Hostname: page-component-848d4c4894-hfldf Total loading time: 0 Render date: 2024-05-29T04:29:26.310Z Has data issue: false hasContentIssue false

Quartz grain surface features in environmental determination of aeolian Quaternary deposits in northeastern Tunisia

Published online by Cambridge University Press:  05 July 2018

A. Chakroun*
Affiliation:
Department of Geology, Faculty of Sciences of Tunis, 2092 El Manar II, Tunisia
J.-C. Miskovsky
Affiliation:
University of Perpignan, UMR 5590 CNRS, CERPT, 66720 Tautavel, France
D. Zaghbib-Turkil
Affiliation:
Department of Geology, Faculty of Sciences of Tunis, 2092 El Manar II, Tunisia

Abstract

Quartz grain surfaces from the Quaternary sand deposits of northeastern Tunisia were examined by scanning electron microscopy. Superficial textures on the quartz grain surface are commonly well preserved and are characteristic of specific formation conditions, allowing the reconstruction of the transport and sedimentation chronology and environment of individual grains.

In the northeastern coastal part of Tunisia (Cap Bon peninsula), the quartz grain exoscopy analysis involves a complex sedimentary history during the Quaternary. The Quaternary dune samples provided a mixture of sub-angular and rounded quartz morphotypes with well preserved mechanical impacts on the grain surfaces. The investigated quartz grains revealed reasonably distinct textural combinations and are characterized firstly, by mechanical features, and secondly, by chemical processes. In all the materials examined, differing environmental evolutions, marine, aeolian and pedologic were detected.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2009

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Chakroun, A. (2006) Etude sedimentologique et paleontologique des affleurements du Quaternaire le long de la cote Nord Orientale de la Tunisie. These de Doctorat, Universite de Tunis El Manar et Universite de Perpignan, 400 pp.Google Scholar
Chakroun, A., Zaghbib-Turki, D., Moigne, A.M. and Lumley, De H. (2005) A Discovery of a Pleistocene mammalia fauna in El Geffel Cave (Cap Bon, Tunisia). Comptes Rendus Palevol, 4, 317—325.Google Scholar
Chakroun, A., Zaghbib-Turki, D., Miskovsky, J.-C. and Davaud, E. (2009) Two Tyrrhenian transgressive cycles in coastal deposits of the Cap Bon Peninsula, Tunisia. Quaternaire, 20, 215—226.Google Scholar
Krinsley, D.H. and Donahue, J. (1968) Environmental interpretation of sann grain surface textures by electron microscopy. Geological Society of America Bulletin, 79, 743—748.10.1130/0016-7606(1968)79[743:EIOSGS]2.0.CO;2CrossRefGoogle Scholar
Krinsley, D.H. and Marshall, J.R. (1987) Sand grain textural analysis: an assessment. Pp. 2—9 in: Clastic Particles. SEM. and Shape Analysis of sedimentary and volcanic clasts (J.R. Marshall, editor). Van Nostrand-Reinhold, NewYork.Google Scholar
Krinsley, D. and Wellendorf, W. (1980) Wind velocities determined from surface textures of sand grains. Nature, 283, 372—373.10.1038/283372a0CrossRefGoogle Scholar
Krinsley, D., Takahashi, T., Silberman, M. and Newman, W. (1964) Transportation of sand grains along the Atlantic shore of Long Island, New York: an application of electron microscopy. Marine Geology, 2, 100—121.10.1016/0025-3227(64)90029-5CrossRefGoogle Scholar
Legigan, Ph. (2002) Application de l’exoscopie des quartz a la reconstitution des environnements sedimentaires. Pp. 859—877 in: Geologie de la prehistoire: Methodes, Techniques, Application. L’association pour l’etude de l’environnement geologique de la prehistoire, Paris.Google Scholar
Legigan, Ph. and Le Ribault L. (1987) Exoscopie des quartz : application a la reconstitution des environnements sedimentaires. Pp. 499—509 in: Geologie de la prehistoire: Methodes, Techniques, Application. L’association pour l’etude de l’environnement geologique de la prehistoire, Paris.Google Scholar
Legigan, Ph., Le Ribault, L. and Miskovsky, J.C. (1989) L’histoire des grains de quartz. Association GEOPRE, Serie de 20 diapos et fasc. Commentaire, 23 pp.Google Scholar
Le Ribault, L. (1975) L’Exoscopie des Quartz. Masson, Paris, 150 pp.Google Scholar
Magee, A.W., Bull, P.A. and Goudie, A.S. (1988) Chemical textures on quartz grains: An experimental approach using salts. Earth Surface processes and landforms, 13, 665—667.CrossRefGoogle Scholar
Margolis, S.V. and Kennett, J.P. (1971) Cenozoic paleoglacial history of Antarctica recorded in subAntarctic deep-sea cores. American Journal of Science, 271, 1—36.10.2475/ajs.271.1.1CrossRefGoogle Scholar
Margolis, S.V. and Krinsley, D.H. (1971) Submicroscopic frosting on eolian and subaqueous sand grains. Geological Society of America Bulletin, 82, 3395—3406.10.1130/0016-7606(1971)82[3395:SFOEAS]2.0.CO;2CrossRefGoogle Scholar
Niftah, S., Debenath, A. and Miskovsky J.C. (2005) Origine du remplissage sedimentaire des grottes de Temara (Maroc) d’apres l’etude des min^raux lourds et l’etude exoscopique des grains de quartz. Quaternaire, 16, 73—83.Google Scholar