LIL:大离子亲石
“Large Ion Lithophile”(大离子亲石元素)常被简写为LIL,以方便在书写和学术交流中快捷使用。这一术语多见于地球化学、地质学等综合性研究领域,通常用于描述一类具有较大离子半径和较强亲石性质的元素,广泛应用于矿物成因和地球演化等相关研究。
Large Ion Lithophile具体释义
Large Ion Lithophile的英文发音
例句
- Its large ion lithophile elements are enriched with obvious Nb, P and Ti negative anomaly and slight Th positive anomaly and low content of Sr.
- 大离子亲石(LIL)元素富集,具明显的Nb、P、Ti负异常和弱的Th正异常,Sr含量较低;
- 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.
- 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(LIL)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。
- 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.
- 微量元素相对富集大离子亲石(LIL)元素,而亏损高场强元素,具有Nb、Ta和Ti异常。
- The syenite is enriched in large ion lithophile elements, radioactive heat-generating elements, high field strength elements and LREE and depleted in Sr and Ba and has weak negative Eu anomalies.
- 岩石富集大离子亲石(LIL)元素、生热元素和轻稀土元素,贫Sr、Ba,具弱的Eu负异常。
- They are relatively enriched in large ion lithophile elements ( Ba and Sr ) and depleted in high field strength elements ( Nb, Ta, Zr and Hf ).
- 富集大离子不相容元素(Ba,Sr),亏损高场强元素(Nb,Ta,Zr,Hf);
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