矿源

他们外出寻找新的矿源。

They went out after new mineral resources .

锂主要存在于锂矿石、海水及盐湖卤水中，而矿石中锂的含量少，品位低，成分杂，从中提取锂成本高，且矿源有限。

Lithium mainly exists in mines , seawater and salt lakes . But it is very difficult and costly to extract lithium from the mineral resources because the minerals are low-grade , heterogeneous and limited .

X射线荧光光谱分析多矿源铁矿石中9种成分

Determination of nine components in various source iron ores by X-ray fluorescence spectrometry

深海沉积的凝缩段是Zn及部分pb的矿源层；

The condensed sequence of deep sea sediments is the major source bed of Pb and Zn .

微量元素、稀土元素和H、O同位素特征表明，白云鄂博群浅变质岩为矿源岩。

The combination characteristics of microelements , REE , H , O isotopes support that metallogenic materials came from the epimetamorphic rocks of Baiyun'ebo Group .

第Ⅲ、Ⅳ旋回玄武岩系（P（2β3）和P（2h））是区内重要的矿源层和赋矿层位。

The basaltic formation of the third and fourth cycle ( P2 β 3 and P2h ) is the important ore Source and ore bed in this district .

金的成矿作用及金矿床的形成，通常与含金丰度相对较高的地台构造层有密切的成因联系，它们提供了重要的物质来源，可认为是矿源层（Sourcebeds）。

Gold metallogenesis and the formation of gold deposits usually have close relationship with the platform strata with relatively high gold abundance . These strata are considered ore-forming material source beds .

地层中Au的丰度值为克拉克值的2～3倍，是形成金矿的矿源层。

The Au abundance in stratum is more 2 or 3 times than Au clarke , thus the Tahua Group is an ore source bed .

成矿流体是具有δCe和δEu负异常的酸性溶液，基本保留了矿源层的稀土分布模式。

The ore fluid was an acidic solution characterized by δ Ce and δ Eu negative anomalies and it basically maintains the REE patterns of the original source bed .

矿源岩中以辉铜矿和黄铜矿最有利于溶解和迁移，NaCl对Cu的溶解和含矿流体的形成起了催化作用。

In source rock , chalcocite and chalcopyrite are favorable minerals to dissolution and transporting of Cu , and NaCl catalyzes dissolution of Cu and formation of Cu-bearing fluid .

寒武纪地层的W、Sn等元素含量较高，是重要的矿源层。后期的热事件使成矿元素发生重新分布。

Precambrian strata which are rich in ore-forming elements such as W and Sn are resource layer of the tin poly-metallic deposit and the geothermal incidents afterwards made these elements redistribute .

红土型金矿具有风化剖面厚度小、成熟度偏低、对矿源体类型及含Au性依赖强、含矿层单一且厚度较小的特点。

The lateritic gold deposits have characteristics of small thickness in weathered section , lower maturity , higher dependence on the gold bearing property and the source body types , singal gold bearing bed of smaller thickness .

论述了Au的矿源体（场）、特定的岩性和地质结构、挽近地史时期的气候和喀斯特地质结构和水动力系统在成矿中的内在联系及其对矿床分布的控制作用。

Discussion on the inherent relation in the ore-forming process of Au involving the original ore body , specific lithologic characters and geological structure , climate in neoid period and karst geological structure and hydrodynamic system and control process with deposit distribution has been carried out .

城市圈层论论元古界矿源层

Urban Circle Layer Discussion ON THE SOURCE-BED OF THE PROTEROZOIC GROUP

通达地幔的深大断裂提供了丰富的矿源和成矿空间；

Great mantle-connected fault supplied plenty of ore source and space ;

矿源场-成矿节-遥感信息异常找矿模式法

Prospecting model method of provenance field-ore_forming NODE-REMOTE sensing anomalies related to mineralization

不同矿源橄榄石对催化苯水蒸气重整的影响

Effects of Olivines from Different Quarries on the Steam Reforming of Benzene

矿源层是成矿作用的物质基础和必备条件。

Source bed is a material base and essential condition of mineralization .

论金属矿床形成的矿源层控制

Ore source bed control and the formation of ore deposit

矿工们往往从矿源较丰富的地方入手。

Miners dig in the better parts of mines first .

金矿床矿源岩分析的新思路

New approaches to study the source rock of gold deposit

浅析湘南地区锰矿矿源物质来源

Primary discussion the origin of Mn ore source material in South Hunan

液态矿源说二次迁移论&内生金矿成矿模式与找矿模型

The Metallogenetic Theory of Gold Deposits : Liquid-Source and It 's Remigration

矿源层为中三叠统浊积岩。

Source beds are turbidite of middle Triassic series .

河北省金的矿源层和地球化学块体

Gold ore source beds and geochemical blocks of Hebei

三类矿源岩石组合提供金质。

The Au is originated from 3 rock assemblages .

巴马丹拿集团论元古界矿源层

On the source - bed of the Proterozoic group

金矿矿源层与矿源层中金的丰度和活度

Abundance and Activity of Gold in the Source Bed

金矿矿源层（岩）研究进展

Progress of research on gold source bed / Rock

矿质、矿源主要来自花岗岩本身，成矿是成岩作用晚期进一步分异的产物。

The mineral source is mainly from granite itself .