| 1. | The determining of the salinity of the ore - forming fluid inclusions using mlrm
成矿流体包裹体盐度的拉曼光谱测定 |
| 2. | Ore - forming fluid rooted in the deep crust mixed with meteoric water
成矿流体来源于地壳深部和后期大气降水的加入。 |
| 3. | Geology and ore - forming fluid types of the linxiang gold deposit , xunyong , shanxi
陕西旬阳淋湘金矿地质特征和成矿流体属性 |
| 4. | Isotopic geochemistry tracing for sources of ore - forming fluid in tianwan ore belt
田湾金矿成矿带成矿流体的同位素地球化学示踪 |
| 5. | 2 . considerable progress has been made in the study of ore - forming fluids
对该区与成矿有密切关系的脉石英进行了成矿流体方面的研究。 |
| 6. | Preliminary discussion on supercritical ore - forming fluid system of zijinshan copper - gold deposit in
初论紫金山铜金矿床超临界成矿流体系统 |
| 7. | Study of short - chain carboxylates in ore - forming fluids of gold - bearing quartz veins in the southeastern guizhou
黔东南某些含金石英脉成矿流体中的短链羧酸 |
| 8. | C . monofunctional carboxylates probably are the important components of meso - high temperature ore - forming fluids
一元羧酸盐可能是中-高温成矿流体中的重要组分。 |
| 9. | The complexity of ore - forming fluid isotopic composition in tianwan gold ore belt implies that the fluid was multi - source
田湾金矿成矿带中，成矿流体同位素组成的复杂性，反映了成矿流体是多源的。 |
| 10. | Homogenization temperature and salinity of ore - forming fluid show some regularity at space , this indicates that ore - forming fluid flow has directivity
成矿流体的均一温度和盐度在空间上都有一定的变化规律，表明成矿演化具有定向性。 |
