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- REE超常富集层super-enriched REE bed
- 碳酸盐岩风化成土过程中REE超常富集及Ce强烈亏损的地球化学机理Formation mechanism of the superhigh concentration of REE and the strong negative Ce anomalies in the carbonate rock weathering profiles in Guizhou Province, China
- 层layer
- 贵州遵义早寒武黑色岩系底部Se的超常富集SUPER-ENRICHMENT OF Se IN THE BOTTOM BLACK SHALES LOWER CAMBRIAN AT ZUNYI, GUIZHOU PROVINCE, CHINA
- 金富集层位enrichment horizon
- 富集层enriched layer
- 单层monolayer
- 黄土坡面细沟侵蚀过程的REE示踪The REE Tracer Method for the Study of Rill Erosion Process on Loess Sloping Surface
- 腐殖质富集层humus enriched horizon
- 微生物及有机酸对风化壳中REE的溶出实验An Experimental Study on the Effects of Microbes and Organic Acids on Dissolution of REE in the Weathering Crust of a Granite
- 内层lining
- 超常的supranormal
- 薄层folium
- 镍-钼富集层Ni-Mo sulfide layer
- 层数number of plies
- 层高height between floors
- 层压lamination
- 层板plywood
- 渔塘坝硒矿区硅质岩的REE总量较低,平均为38.9×10~(-6),紫阳硒富集区硅质岩REE总量除个别较高(达110×10~(-6)以上)外,总体也较低(12.0-37.6)×10~(-6);In Yutangba selenium deposit, the REE content of siliceous rocks is Iow(38.9x10-6), and enriched in LREE. In Ziyang selenium-rich area, it is from (12.0-37.6)x10-6, In both of two areas, there exist Ce negative anomaly and Eu positive anomaly.
- 层的stratal