lile meaning in English
侧带鲱属
等大离子亲石
离子亲石性元素
离子亲石元素
莉列
利莱
Examples
- Outgoing and practical person . i lile swimming and outdoors . honest and sometimes romantic . my ideal partner should be good tempered and filial to parents . thats my only requirement
我是个对人友好并且实际的人.我喜欢游泳和外出.正直和浪漫.我理想的人是一个很会调节的,孝顺父母的人.这就是我的要求 - Two ree distributed pattern , lree - depleted and flat , which display a specific character of typical mid - ocean ridge tholeiite , indicate that primary magma may be derived from near primary or a typical large ion lithophile element ( lile ) - depleted mantle
岩石稀土元素配分模式可分为lree平坦型和lree亏损型两类，指示了其原始岩浆起源于近原始或典型的大离子元素亏损型的地幔，为典型的大洋中脊拉斑玄武岩的特征。 - The southern hainan mafic dykes are strongly enriched in lile with high nb / ta ratios , indicating a magma source reconstructed by silicic - melt through partial melting of ancient subducted slides . however , the northern hainan mafic dykes with chondritic nb / ta ratio should be derived from the fiuid - metasomatized mantle related to ancient subduction zone
琼南基性岩脉强烈富k _ 2o等lile和具有较高nb ta比值，其地幔源区应受到了古俯冲板片部分熔融形成的硅质熔体的改造；而琼中基性岩脉的nb ta比值接近于球粒陨石和morb值，应为古俯冲带含水流体交代的地幔源区的产物。 - The geochemical data of the benzilan and pantiange volcanic rocks from the jinshajiang zone yielded characteristics similar to those of island - arc volcanic rocks : intensive enrichment in lile and different depletion in hfse , nb , ta , ti , p and zr , hf . their lower e nd ( t ) values ( - 4 . 03 - - 11 . 29 ) indicate that they are derived from an emu mantle source or a mixing source between dm and emu respectively , but which are affected violently by subduction materials
同位素研究显示，它们具有较低的_ ( nd ) ( t )值( - 4 . 03 - 11 . 29 ) ，表明它们分别来源于富集地幔emii以及亏损地幔dm和emii两元混合的源区，两地的火山岩源区都受到了俯冲带物质的强烈影响。 - 2 both the hanging wall and the footwail rock of ore bodies are garnet biotite schist , protoliths are alkaline volcanic rocks ( tracyh andesite ) . according to characteristics of trace elements assemblages and the setting of tectonics , these alkaline volcanic rocks were derived from the lower degree melting of metasomatic and enriched mantle ( eml ) in the initial stage of middle proterozoic epoch . they strongly enriched in large ion lithophile elements ( lile ) , such as ba
2 、矿体顶、底板围岩(石榴石黑云母片岩、钠长黑云母片岩等)的原岩为碱性火山岩(粗面安山岩) ，相对富集大离子亲石元素ba 、 cs 、 rb 、 k 、 lree及贫zr 、 sr 、 ti 、 hf 、 hree ，为早元古代末期-中元古代早期交代富集地幔低程度部分熔融所形成的碱性火山岩。