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- W2387831405 abstract "Rock records indicate that largescale sand desertification dates back to middle Mesozoic Era, that there has existed a middle latitude sand desert zone in the south and north hemispheres respectively since Quaternary Period, and that sand desertification in China is a part of global sand desertification process. Sand desertification, controlled by internal and external dynamic geological processes in the geological evolution, is a special geological phenomenon imposed by the interaction of lithophere, atmosphere, biosphere, and hydrosphere on the surface layer of the earth's crust. The evolution of sand desertification, which is long and periodic, won't undergo a sudden change in a whole sense because of partial condition change. Human activity is regionally restricted, serving as an accelerator in the global sand desertification. The process of sand desertification can be divided into 3 stages: physical weathering and accumulation of sand source stage; windblown and sandblast stage; sand desertification stage. The windformed sandstone was formed by the dune after solidifygrassing and cementationdiagenesis stages." @default.
- W2387831405 created "2016-06-24" @default.
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- W2387831405 date "2003-01-01" @default.
- W2387831405 modified "2023-09-25" @default.
- W2387831405 title "Research on geneses of sand desertification from dynamic geological processes" @default.
- W2387831405 hasPublicationYear "2003" @default.
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