Geoscience Reference
In-Depth Information
McKenna Neuman, C., Lancaster, N. and Nickling, W.G. (1997)
Relations between dune morphology, air flow, and sediment
flux on reversing dunes, Silver Peak, Nevada.
Sedimentology
,
44
, 1103-1113.
Mahmoudi, F. (1977) Les nebkhas de Lut, Iran.
Annales de
Geographie
,
77
, 296-322.
Mainguet, M. (1968) Le Bourkou - Aspects d'un modele eolien.
Annales de Geographie
,
77
, 296-322.
Mainguet, M. (1970) Un etonnant paysage: les cannelures
greseuses du Bembeche (N. du Tchad). Essai d'explication
geomorphologique.
Annales de Geographie
,
79
, 58-66.
Mainguet, M. (1972)
Le Model´edesGres
, Institute Geographie
National, Paris.
Mainguet, M. (1996) The Saharo-Sahelian global wind action
system: one facet of wind erosion analysed at a synoptic
scale, in
Wind Erosion in West Africa: The Problem and Its
Control
(eds B. Buerkert, B.E. Allison and M.V. Oppen),
Proceedings of the International Symposium, University of
Hohenheim, Germany, 5-7 December 1994, Weikersheim,
Germany, pp. 7-22.
Maizels, J.K. (1987) Plio-Pleistocene raised channel systems of
the western Sharqiya (Wahiba), Oman.
Geological Society,
London, Special Publications
,
35
, 31-50.
Maxson, J.H. (1940) Fluting and faceting of rock fragments.
Journal of Geology
,
48
, 717-751.
Mildrexler, D.J., Zhao, M. and Running, S.W. (2006) Where
are the hottest spots on Earth?
EOS, Transactions of the
American Geophysical Union
,
87
, 461-467.
Mulligan, K.R. (1988) Velocity profiles measured on the wind-
ward slope of a transverse dune.
Earth Surface Processes
and Landforms
,
13
, 573-582.
Neev, D. and Hall, J.K. (1992) Counterclockwise converging
basement fracturing patterns across the Arabian Peninsula
and Eastern Iran, in
Basement Tectonics
(ed. R. Mason),
International Basement Tectonics Association Publication 7,
pp. 13-31.
Nero, R.W. (1988) The ventifacts of the Athabasca sand dunes.
The Musk Ox
,
36
, 44-50.
Powers, W.E. (1936) The evidences of wind abrasion.
Journal
of Geology
,
44
, 214-219.
Ritley, K. and Odontuya, E. (2004) Yardangs and dome dunes
northeast of Tavan Har, Gobi, Mongolia, Geological Society
of America Abstract with Programs: Rocky Mountain and
Cordilleran Joint Meeting, vol. 36, p. 33.
Scattergood, R.O. and Routbort, J.L. (1983) Velocity exponent
in solid-particle erosion.
Journal of the American Ceramic
Society
,
66
, C184-C186.
Schlyter, P. (1994) Paleo-periglacial ventifact formation by sus-
pended silt or snow. Site studies in south Sweden.
Ge-
ografiska Annaler, Series A, Physical Geography
,
76A
,
187-201.
Schoewe, W.H. (1932) Experiments on the formation of wind-
faceted pebbles.
American Journal of Science
,
24
, 111-
134.
Schwanghart, W. and Schutt, B. (2008) Meteorological causes
of Harmattan dust in West Africa.
Geomorphology
,
95
,
Selby, M.J. (1977) Palaeowind directions in the central Namib
Desert, as indicated by ventifacts.
Madoqua
,
10
, 195-198.
Sharp, R.P. (1949) Pleistocene ventifacts east of the Big
Horn Mountains, Wyoming.
Journal of Geology
,
57
, 173-
195.
Sharp, R.P. (1964) Wind-driven sand in Coachella Valley, Cal-
ifornia.
Bulletin of the Geological Society of America
,
75
,
785-804.
Sharp, R.P. (1980) Wind-driven sand in Coachella Valley, Cal-
ifornia: further data.
Bulletin of the Geological Society of
America
,
91
, 724-730.
Smith, H.T.U. (1963) Eolian geomorphology, wind direction,
and climatic change in North Africa, Air Force Cambridge
Reseach Laboratories, Bedford, MA, AFCRL - 63-443,
48 pp.
Smith, H.T.U. (1967) Past versus present wind action in the
Mojave Desert region, California, Air Force Cambridge Re-
search Laboratories, 67-0683, pp. 1-26.
Smith, R.S.U. (1984) Eolian geomorphology of the Devils
Playground, Kelso Dunes and Silurian Valley, California,
in
Western Geological Excursions. Vol. 1: Geological Soci-
ety of America 97th Annual Meeting Field Trip Guidebook,
Reno, Nevada
(ed. J. Lintz), Geological Society of America,
pp. 239-251.
Songqiao, Z. and Xuncheng, X. (1984) Evolution of the Lop
Desert and the Lop Nor.
The Geographical Journal
,
150
,
311-321.
Stapff, F.M. (1887) Karte des unteren Khuisebtals.
Petermanns
Geographische Mitteilungen
,
33
, 202-214.
Sun, J. (2002) Source regions and formation of the loess sedi-
ments on the high mountain regions of northwestern China.
Quaternary Research
,
58
, 341-351.
Taylor, P.A. (1977) Numerical studies of neutrally stratified
planetary boundary-layer flow above gentle topography.
Boundary-Layer Meteorology
,
12
, 37-60.
Todd, M.C., Washington, R., Martins, J.V.
et al.
(2007) Mineral
dust emission from the Bodele Depression, northern Chad,
during BoDEx 2005.
Journal of Geophysical Research
,
112
,
D06207, DOI: 10.1029/2006JD007170.
Tremblay, L.P. (1961) Wind striations in northern Alberta and
Saskatchewan, Canada.
Bulletin of the Geological Society of
America
,
72
, 1561-1564.
Tsoar, H. (1985) Profiles analysis of sand dunes and their steady
state signification.
Geografiska Annaler
,
67A
, 47-61.
Twidale, C.R. (1994) Desert landform evolution: with special
reference to the Australian experience.
Cuaternario y Geo-
morfologıa
,
8
, 3-31.
Vincent, P. and Kattan, F. (2006) Yardangs on the Cambro-
Ordovician
Saq
Sandstones,
North-West
Saudi
Arabia.
Zeitschrift f ur Geomorphologie
,
50
, 305-320.
Ward, A.W. and Greeley, R. (1984) Evolution of the yardangs at
Rogers Lake, California.
Bulletin of the Geological Society
of America
,
95
, 829-837.
Washington, R. and Todd, M.C. (2005) Atmospheric controls on
mineral dust emission from the Bodele Depression, Chad: the
role of the low level jet.
Geophysical Research Letters
,
32
,