成矿的

The circulation of volcanic hot spring formed the alteration zone which, together with atmospheric water and subvolcanic hydrothermal solution, formed micro-crystalline quartz that contained adular and sericite.

火山热泉循环形成蚀变晕，此阶段有大气降水的参与；潜火山热液成矿阶段发育的低温微细石英网脉中含冰长石和绢云母。

All the deposits have the same associations of ore-forming elements, auriferous minerals and alterations.

金矿床具有基本相同的成矿元素组合和主要的载金矿物和围岩蚀变组合。

Fracturing of mineralization stage is found mainly concentrated in the early quartz veins or the hydrofracturing breccia in the sandy tectonic lenses, the lens-like orebody mainly consisting of the cataclastic quartz veins and hydrofracturing breccia form.

成矿阶段的破裂主要集中在砂岩构造透镜体中早期石英脉或液压角砾岩上，形成以碎裂石英脉及液压角砾岩为主要矿化母岩的透镜状矿体。

Because of obstruct of the earth surface or concentration effect, these elements can be left in the earth surface. Investigating these migratory elements helps to find out delitescent mines.

随地气和地下水蒸发而迁移的成矿元素，因地表覆盖层的阻隔作用或因浓缩作用，会卸载于地表覆盖层中。

Sandstone type uranium ore is a epigenetic hydrogenic uranium deposit, and its mineralizing theory is mainly on the basis of the hydrogeology and hydrogeochemistry, and many key problems need to explore in the course of uranium ore-forming have closely to do with hydrogeochemistry.

砂岩型铀矿是一种后生水成铀矿床，其成矿理论是建立在水文地质学、水文地球化学等学科基础上，矿床形成中的许多有待探索的关键问题都与水文地球化学密切相关。

Thermometric measurements of inclusions in quartz have provided evidence for mesothermal hypothermal origin of the Baguamiao gold deposit.

同时，为八卦庙金矿的成矿提供了条件。石英中包裹体测温结果为八卦庙金矿床的中温成因提供了证据

Mao Jingwen%Wang Zhiliang%Li Houmin%Wang Chengyu, Chen Yuchuan Carbon and oxygen isotope components in the Permian basalt-hosted copper deposit in Ludian area, Yunnan:Implication for the mineralization process Geological Review , 2003,6

毛景文%王志良%李厚民%王成玉%陈毓川云南鲁甸地区二叠纪玄武岩中铜矿床的碳氧同位素对成矿过程的指示地质论评， 2003，6

We consider the ore fluid consists of meteoric water and magmatic water.

认为成矿流体既有来自花岗闪长岩体的岩浆水参与，又有大气降水的作用。

It is believed that the metallogenic hydrothermal system of this deposit is a mixture one formed by magmatic and reformatiom hydrothermal fluids.

本文以云南元阳金矿床为例探讨了该矿床的成矿热液系统的地球化学特征。

Fluid inclusion studies of ten mesothermal gold deposits in Tongbo-Dabie area show that the ore-forming fluids are of the NaCl-CO2-H2O system with low salinity (6 wt%NaCl) and ricb CO2 (10 mol%).

中文摘要：通过对桐柏-大别地区10个中温热液金矿床的流体包裹体研究，确定成矿流体属于低盐度（6 wt% NaCl）、富CO2 (10 mol%)的NaCl-CO2-H2O体系。

According to the clear water experiment, aeration performance of the new equipment is good with high total oxygen transfer coefficient and oxygen utilization ratio.

曝气设备的动力效率在叶轮转速为120rpm～150rpm时取得最大值，此时氧利用率和充氧能力也具有较高值。

The environmental stability of that world - including its crushing pressures and icy darkness - means that some of its most famous inhabitants have survived for eons as evolutionary throwbacks, their bodies undergoing little change.

稳定的海底环境─包括能把人压扁的压力和冰冷的黑暗─意谓海底某些最知名的栖居生物已以演化返祖的样态活了万世，形体几无变化。