富成

云南中部富碱斑岩成岩成矿的大地构造控制作用

Tectonic control for Petrogenesis and metallogenesis of the alkali rich porphyries in Central Yunnan

滇西新生代富碱火成岩及其与金成矿关系研究

The Cenozoic Alkali-rich Igneous Rocks , Western Yunnan and Their Relation with Metallogenesis of Gold

白马寨镍矿区煌斑岩位于哀牢山断裂带的南段，是该条带上新生代富钾火成岩的重要组成部分。

Lamprophyres in the Baimazhai nickel deposit are located on the southern segment of Ailaoshan fault belt .

要牢牢的抓住这确实的把握，就是神要丰丰富富的作成一切超过我们所求所想的。

Hold fast the confident assurance that God will do abundantly above what we can ask or think .

控制深盆气富气区块成藏机理的动力是气体膨胀力、毛细管力和浮力，它们在深盆气富气区块成藏过程的不同阶段具有不同的表现和控制作用。

The controlling forces include gas expanding force , capillary pressure and buoyancy , which play different roles during different stages .

地幔流体在滇西富碱斑岩成岩成矿过程中的作用&地质年代学和同位素地球化学制约

Mantle Fluid 's Action in the Processes of Petrogenesis of Alkalic Porphyry and Associated Mineralizations , Western Yunnan , China-Constraint of Geochronology and Isotope Geochemistry

从而建立了实验条件下较完整的深盆气富气区块成藏序列及成因机理模式。

Thus , relatively complete accumulation succession and mechanism model of deep basin gas accumulation and its high-permeability gas-rich zone under physical laboratory condition are established .

聂云台《保富法》成书于新中国解放前夕，是中国佛教哲学史上一部重要学术著作。

" Law of Retaining Wealth " was written by Yun-tai Nie on the eve of the liberation of New China , which is an important academic works in the history of Chinese Buddhism philosophy .

使用电镜和FTIR光谱仪表征了不同结构富碳有机物成炭的表观形貌。

The appearances of the carbon made from the organics rich in carbon are displayed by the SEM and FTIR respectively .

通过对富碳有机物成炭方法、机理进行分析和研究，提出了富碳有机物成炭机理图。

The carbonization mechanism map of the organics rich in carbon is deduced through the study and the analysis of the carbonization method and mechanism of the organics rich in carbon .

据此，从地幔流体交代矿物的结晶年龄（116.0Ma）到富硅成矿流体年龄（51.2Ma），揭示地幔流体作用贯穿于富碱岩浆成岩成矿的全过程。

The mineral crystalline age ( 116.0 Ma ) of the mantle fluid metasomatism and the age ( 51.2 Ma ) of the silicon-rich mineralizing fluid suggest that the mantle fluid had been active through the whole processe of the alkalic magma diagenism and associated mineralization .