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1.The dips are 25°~30° with uniformly dip directions. The lamina of cross?bedding is thinning upward with reverse grading and tangential to the lower bounding surfaces. The bounding surfaces are generally wavy eolian erosion surfaces with high wave index(>15).
风成证据有:(1)普遍具风成大型交错层理,倾角达20°~30°且倾向均一,交错纹层向上变薄,具反粒序,与下伏界面相切,层间界面多为高波痕指数(>15)波状风蚀起伏面。收藏指正
2.On Resistance of Eolian Sandy Soil Moisture to Wind Erosion
风沙土水分抗风蚀性研究收藏指正
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