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la ria de Huelva à l’embouchure du Guadalquivir). Mélanges de la Casa Velâzquez, 1979,
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© a r m a n d
c o l in .
L a
p h o to c o p ie n o n
a u to ris é e e s t u n délit..
99
Sherman D.J. et Bauer B.O. — Dynamics of beach-dune sustems. Progress in Physical
Geography, 1993,17, 413-447.
Sherman D.J. et Hotta S. — Aeolian sédiment transport : theory and measurement. Coastal
dunes, form and process, K.F. Nordstrom, N. Psuty et B. Carter édit. Wiley, Chichester,
1990,17-55.
Sherman D.J. et Nordstrom K.F. — Hazards of wind-blown and Coastal sand drifts : a review.
Coastal hazards, perception, susceptihility and mitigation, C.W. Finkl édit., Journal of
Coastal Research, 1994, n° spécial 12, 263-275.
Svasek J. N. et Terwindt J.H.J. — Measurements of sand transport by wind on a natural beach.
Sedimentology, 1974, 27, 311-322.
Thomas Y. F. — Actions éoliennes en milieu littoral. La pointe de la Coubre. Mém. Lah.
Géomorph. E.P.H.E., 1975, 29, 202 p.
Tinley K.L. — Coastal dunes of South Africa. Foundation for Research Development, Prétoria,
1985, 297 p.
Vanney J.R. et Menanteau L. — Types de reliefs littoraux et dunaires en Basse-Andalousie (de
la ria de Huelva à l’embouchure du Guadalquivir). Mélanges de la Casa Velâzquez, 1979,
75,5-52.
© a r m a n d
c o l in .
L a
p h o to c o p ie n o n
a u to ris é e e s t u n délit..
