高场强元素

  • 网络high field strength element;HFSE
高场强元素高场强元素
  1. 富集大离子不相容元素(Ba,Sr),亏损高场强元素(Nb,Ta,Zr,Hf);

    They are relatively enriched in large ion lithophile elements ( Ba and Sr ) and depleted in high field strength elements ( Nb , Ta , Zr and Hf ) .

  2. 微量元素相对富集大离子亲石元素,而亏损高场强元素,具有Nb、Ta和Ti异常。

    The trace elements of the mafic dikes are characterized by relative enrichment of large ion lithophile elements and depletion of high field strength elements , and negative Nb and Ta and Ti anomaly .

  3. 南北两带岩体均富集轻稀土元素、大离子亲石元素和高场强元素,而Cr、Ni等相容元素含量很低。

    Both belts are enriched in LREE , large_ion lithophile elements and high charge density elements . However , the content of compatible elements such as Cr and Ni are very low .

  4. 矿石与围岩的微量元素研究表明:Mo、V、Pb等微量元素强烈富集而大离子与高场强元素含量很低;

    The research on ore and ore-bearing rock trace elements indicate that Mo , V , Pb elements are remarkably enriched , whereas high field strength elements and lithophile elements are very low .

  5. 高场强元素(HFSE)相对相邻REE的亏损程度随LREE富集程度的增大而增大。

    The degree of depletion of high field strength elements ( HFSE ) relative to the neighbouring REE increases with the LREE enrichment .

  6. 在17种元素的标准化曲线图上,具Rb、K的峰和Ta、Ti的谷,表明了火山岩中大离子半径元素的相对富集和高场强元素的贫化。

    In the chondrite-normalized multiple-element diagrams ( spidergram ) the peaks at K and Rb and the troughs at Ta and Ti have been observed , which indicate relative enrichment of K-group elements and depletion of some HFS elements in the volcanic rocks .

  7. 上述岩石包体与寄主岩相比,相对地富Zr,P,Ti和REE等高场强元素,这说明发生混合的、成分不同的两岩浆很可能是同源的,由液相不混溶作用产生。

    The fact that the enclaves and the host rock are comagmatic and that the former is relatively rich in high-field-strength elements such as Zr , P , Ti , REE , etc. suggests that origin of the enclaves may be magma immiscibility between the two corresponding magmas .

  8. 对于蚀变岩的多原岩系统,常用不相容高场强元素(HFSE)来描述岩石性质,用其作为监视器,可作出各相容元素(或成分)的分异线;

    The incompatible high field strength elements ( HFSE ) are used as a monitor for multiple precursor systems and for drawing a fractionation line .

  9. 微量元素含量变化大,但总体变化趋势一致,即表现出大离子亲石元素(LILE)富集而高场强元素(HFSE)亏损。

    The intermediate rocks contain variable contents of trace elements , but generally have a similar variation trend such as systematic enrichment of LILE and depletion of HFSE .

  10. 论文通过对玄武岩地球化学的研究,发现营城组玄武岩富集大离子亲石元素和高场强元素,轻重稀土分异强烈,无Nb负异常,显示与OIB类似的地球化学特征。

    These basalts are characterized by enriched large ion lithophile elements and high field strength elements , strong fractionation between light and heavy rare earth elements , no negative Nb anomaly , that resemble to geochemical characters of ocean island basalts .

  11. 与熔融母岩相比,其稀土元素和高场强元素含量相对较低,但大多数情况下具有相似的元素分布模式。

    The anatectic derivatives have lower REE content and HFS elements than their melting parent rocks . In most cases , however , they show similar element distribution patterns .

  12. 高场强微量元素含量与相关比值与一般基性岩相似;

    HFSE and related ratios are similar to those of common basic rocks .

  13. 富铌的岛弧玄武岩则是中等到高碱的镁铁质熔岩,它们相对于正常的岛弧玄武岩含有较多的高场强元素(HFSE)。

    Niobium-enriched arc basalts are mildly - to highly-alkalic mafic lavas that contain relatively higher amount of high field-strength elements ( HFSE ) than normal arc lavas .