Sources of non-glacial, loess-size quartz silt and the origins of “desert loess”-Reference-Cited by-同舟云学术

Sources of non-glacial, loess-size quartz silt and the origins of “desert loess”

Published:2002-11 Issue:1-4 Volume:59 Page:1-26
ISSN:0012-8252
Container-title:Earth-Science Reviews
language:en
Short-container-title:Earth-Science Reviews

Author:

Smith B.J.,Wright J.S.,Whalley W.B.

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences

Reference166 articles.

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2. Spalled quartz overgrowths and their implications for how a sand is derived from a sandstone and vice versa;Anderhalt;Micron and Microscopia Acta,1984

3. The effects of chemical weathering on the morphology and strength of quartz grains—an example from S.W. Australia;Asamudu;Journal of Soil Science,1988

4. Silt: 2–62 μm, 9-4ø;Assallay;Earth-Sciences Reviews,1998

5. Aeolian deposition and soil parent material in northern Nigeria;Bennett;Geoderma,1980

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