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• W1410368296 abstract "Loess consists essentially of silt-sized (typically 20–30 microns) primary quartz particles that form as a result of high-energy earth-surface processes such as glacial grinding or cold-climate weathering. These processes have resulted in an almost continuous deposit from the North China plain to southeast England, for example, although it is possible to isolate five major regions: North America, South America, and Europe including western Russia, Central Asia, and China. These loess regions underlie highly populated areas and major infrastructure links, and are prone to collapse, causing subsidence. The areas of most widespread concern are concentrated in Eastern Europe and Russia and, to a growing extent, in China although serious problems of potential collapse exist wherever loess is found." @default.
• W1410368296 created "2016-06-24" @default.
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• W1410368296 date "2015-01-01" @default.
• W1410368296 modified "2023-09-24" @default.
• W1410368296 title "Improvement of Collapsible Loess in Eastern Europe" @default.
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• W1410368296 doi "https://doi.org/10.1016/b978-0-08-100698-6.00007-6" @default.
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