热液矿物

沉淀过程中热液矿物和热液相比应相对富集Eu和Ce，并再次发生轻重稀土的分馏。

The deposited hydrothermal minerals are richer in Ce and Eu than the solution , and a second fractionation between HREE and LREE occurs during the process of minerals deposition .

水系沉积物Mo、Cu、Pb、Zn稳定组合异常与重砂测量高温热液矿物组合异常的重叠部分可作为成矿母岩与工业钼矿体的推断依据。

The overlapping parts between the stable combination anomaly of stream sediment survey of Mo , Cu , Pb , Zn and the hypothermal mineral combination anomaly through heavy fraction surveying can be taken for foundation to infer mineralization mother rocks and industrial ore bodies .

从太平洋中部热液矿物的发现探讨热液活动的广泛性

A Preliminary Discussion on the Extensiveness of Hydrothermal Activity Based on the Discovery of Hydrothermal Minerals in Cantral Pacific Ocean

矿石由黄铁矿、闪锌矿、自然金、辉锑铅矿、砷黝铜矿、辉锑矿、辉锑银铅矿、雄黄、雌黄等组成，为典型的低温热液矿物组合。

Ores consist of pyrite , blende , aurum , zinckenite , tennantite , antimonite , realgar , and orpiment , belong to typical Low-temperature minerals assemblage .

已有热液矿床矿物流体包体数据表明：有一批矿床的主要矿石形成于300~500℃，低于NaClH2O溶液临界线的条件。

The fluid inclusion data demonstrate that the majority of hydrothermal ores are precipitated in the temperature range of 300 to 500 ℃, lower than the critical line of NaCl-H2O .

热液矿床矿物微形貌与晶体生长环境研究

The surface micromorphology of minerals in hydrothermal ore deposits and growth environments of crystal

在着重分析与金银矿床有关的几种热液蚀变矿物的反射光谱特征的基础上，对采用的波段比值方法做了进一步的阐述。

It was emphasized to analyse a few reflective spectrum characteristics of the hydrothermal altered minerals .

钾质白云母是铅锌银矿床中的主要热液蚀变矿物，通常表现为白云母化、绢云母化、伊利石化。

Potash micatization is one of the main hydrothermal alteration minerals genetically related to the lead-zinc-silver deposit .

浙东南地区与金银矿床有关的几种热液蚀变矿物反射光谱特征及其信息提取

Spectral characteristics of reflectance and information extraction of a few hydrothermal alteration minerals on Au-Ag deposit in east-south area of Zhejiang Province

透辉石为典型的热液接触变质矿物，系花岗岩浆与钙质白云岩接触交代的产物。

Diopside is a typical kind of hydrothermal-metamorphic deposits . It is Formed while contacting with and replacing of granite magma and dolomite .

某些石英脉型热液矿床的矿物流体包裹体压碎浸取和离子色谱分析确定，成矿流体中存在少量短链羧酸，而且甲酸是优势物种。

Crush leaching and ion chromatographic analysis of fluid inclusions in minerals from some quartz vein hydrothermal deposits show that small amounts of formate and acetate are present in most ore fluids and that formate is a dominant species .

流出的热液可以形成多种矿物沉积，其中最有价值的是Zn，Cu，Fe，Pb的硫化物。

The effusive hydrothermal activity can form multi mineral deposits including Zn , Cu , Fe , Pb and sulfides which are the most valuable .

深海热液喷口微生物对矿物元素行为的影响

Influence of microorganisms in deep-sea hydrothermal vents on the behavior of mineral elements

热水溶液中的物种形成（热液流体中的矿物溶解度测定、电势测量和谱学研究）；

Speciation in hydrothermal solutions ( mineral solubility determination , potentiometric and spectroscopic study of hydrothermal fluids );

苏州阳山高岭土矿床中玻屑、低温热液和蚀变矿物的发现以及对矿床成因的新认识

Discovery of VITROCLASTIC ash and minerals of low-temperature hydrothermal alteration of Yangshan kaolin deposit , suzhou , and new understanding of its genesis

根据热液脉体及其矿物特征等，分析了成矿热液演化与控矿构造活动之间的关系。

According to the features of hydrothermal veins and minerals , relationships between the evolution of ore-forming solution and the activities of ore-controlling structures are explained .