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Geomorphic indicators of Holocene winds in Egypt's Western Desert

Brookes, Ian A.·2003·Geomorphology

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Crossref · 10.1016/s0169-555x(03)00076-x

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Research works printed but not linked: 35

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  14. Goodfriend, 1991, Holocene trends in ∂18O in land snail shells from the Negev Desert and their implications for changes in rainfall source areas, Quat. Res., 35, 417, 10.1016/0033-5894(91)90054-9 · DOI
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  22. Maley, 2000, Last glacial maximum lacustrine and fluviatile formations in the Tibesti and other Saharan mountains, and large-scale climatic teleconnections linked to the activity of the Subtropical Jet Stream, Glob. Planet. Change, 26, 121, 10.1016/S0921-8181(00)00039-4 · DOI
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  31. Shahin, 1985, Hydrology of the Nile Basin, vol. 21
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  33. Sultan, 1997, Precipitation source inferred from stable isotopic composition of Pleistocene groundwater and carbonate deposits in the Western Desert of Egypt, Quat. Res., 48, 29, 10.1006/qres.1997.1907 · DOI
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Metadata

Authors
Brookes, I. A.
Venue
Geomorphology
Publisher
Elsevier BV
Published
2003-11
Volume
56
Issue
1-2
Pages
155-166
ISSN
0169-555X
Cited by
50
References
0
Language
en

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