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- REE超常富集層super-enriched REE bed
- 碳酸鹽巖風(fēng)化成土過(guò)程中REE超常富集及Ce強烈虧損的地球化學(xué)機理Formation mechanism of the superhigh concentration of REE and the strong negative Ce anomalies in the carbonate rock weathering profiles in Guizhou Province, China
- 層layer
- 貴州遵義早寒武黑色巖系底部Se的超常富集SUPER-ENRICHMENT OF Se IN THE BOTTOM BLACK SHALES LOWER CAMBRIAN AT ZUNYI, GUIZHOU PROVINCE, CHINA
- 金富集層位enrichment horizon
- 富集層enriched layer
- 單層monolayer
- 黃土坡面細溝侵蝕過(guò)程的REE示蹤The REE Tracer Method for the Study of Rill Erosion Process on Loess Sloping Surface
- 腐殖質(zhì)富集層humus enriched horizon
- 微生物及有機酸對風(fēng)化殼中REE的溶出實(shí)驗An Experimental Study on the Effects of Microbes and Organic Acids on Dissolution of REE in the Weathering Crust of a Granite
- 內層lining
- 超常的supranormal
- 薄層folium
- 鎳-鉬富集層Ni-Mo sulfide layer
- 層數number of plies
- 層高height between floors
- 層壓lamination
- 層板plywood
- 漁塘壩硒礦區硅質(zhì)巖的REE總量較低，平均為38.9×10~(-6)，紫陽(yáng)硒富集區硅質(zhì)巖REE總量除個(gè)別較高(達110×10~(-6)以上)外，總體也較低(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.
- 層的stratal
