成矿的

A series of NW-SE-trending faults and reverse"S"anticlinal bulge in central depression zone between north center fault and south center fault, which are main position of celestite deposits, come into being storage ground of celestite deposits.

中央断块内一系列北西向张性断裂和大量的反"S"型背斜构造带是锶矿的主要定位场所，形成了成矿系统的储矿场。

Cryptical blasting, fluid boiling and meteoric water mixing are reasons of gold deposition in the deposit, forming cement type and vein type mineralisation .

由于角砾岩体的隐爆、流体减压沸腾及古大气水的混入，热液中的金被沉淀成矿，形成胶结物型和脉型金矿化。

The ore deposit remote sensing geology is an interdisciplinary study of gitology and remote sensing geology,which syncretizes the methods of deposit geology and remote sensing geology to identify the inherent relationship between deposit characters and remote sensing information,distinguish the linear and ring structures and their grade system from numerous and complicated lineaments and rings,extract exploration information of tectonic,intrusive body,tectonic denude station and week geology information,such as alteration, special rock and so on.

矿床遥感地质学将矿床学与遥感地质学、矿床地质方法与遥感地质方法相融汇，从成矿地质环境、矿床展布规律及矿床特征出发，识别矿床特征与遥感信息之间的内在联系，厘定纷繁复杂的线性构造、环形构造以及它们之间的组合关系和等级体制，提取构造、侵入体、构造剥蚀程度以及遥感数据中地质弱信息(蚀变信息、特殊岩性信息等)等找矿信息，为快速圈定勘探靶区提供依据。

Hongqiling Cu, Ni sulphide deposit is located in ca. 45km south of Panshi city, Jilin province. It is also situated tectonically in the Tieling contact zone between Jihei geosyncline and Liaodong syncline in North China plate, which is divided by Huifahe fault.

红旗岭铜镍硫化物矿区位于吉林省磐石市南约45Km，地处吉黑地槽与华北台块辽东台背斜铁岭台凸接触地带，辉发河断裂是其分界线，特殊的构造位置决定了本区的构造活动强烈，岩浆活动发育，具备良好的成矿环境和条件。

Combined with related rare earth element and trace element geochemistry of Huangshaping granites and ore-bearing skarn, it is concluded in this paper that the age of 154 Ma should represent the metallogenic epoch of the deposit, and that there existed a close relationship between the ore-forming process of the deposit and the granite porphyry, which were both formed during the peak stage of Early Yanshanian large-scale rock-forming and ore-forming activities in South China.

结合黄沙坪岩体及含矿硅卡岩型矿体的稀土及微量元素地球化学特征，得出以下认识：该矿床的成矿年龄在154Ma左右；成矿作用与花岗斑岩关系密切，它们都是华南燕山早期大规模成岩成矿作用高峰期的产物。

This process (mylonitization, migmatization and granitization) leads to mobilization and migration of gold.

深层次推覆构造带为一复杂的花岗质岩石的成岩带和金等有色矿产的成矿带。

The key reason for no mineralizations aroud the granodiorite intrusions is that they experienced very poor differentiation, and that they were too small in volume to form the hydrothermal brine deposits.

花岗闪长岩之所以没有成矿，关键在于本身的分异程度太低，它们较小的体积，也不足以引起地下热卤水矿床的产生。

There are two direct factors for notion about the difference of occurrence of Se, that is sulfurcontent in the kerogen and the condition of redox.

两种不同的赋存状态可能主要取决于干酪根中硫含量的多少以及成矿时氧化还原条件的变化。

Taking Lehua manganese deposit as an example, geological characters and ore-forming condition s of lower phosphorus high-quality manganese ores in the southeast margin of Yangzi Platform is preliminarily discussed.

文章以乐华锰矿床地质特征为例，初探了扬子地台东南缘低磷优质锰矿的地质特征和成矿条件，并对在赣东北地区寻找该类型矿床的前景提出了自己的看法。

Molybdenum deposits generally occur in nearly E-W direction along the tectonic lineament and are mostly concentrated in a zone stretching from Jinduicheng area of Shaanxi Province in the west to Nannihu-Sandaozhuang-Shangganggou area of Luanchuan and Leimenggou of Songxian in western Hena...

研究结果表明：除黄龙铺钼矿床形成于(221.5±0.3)Ma外，东秦岭地区钼矿床的大规模成矿主要出现在(144.8±2.1)~(132.4±2.0)Ma时限之间，对应的地球动力学背景为华北克拉通与扬子克拉通的碰撞造山后陆内造山局部伸展过程、中国东部地球动力学体制大转换晚期岩石圈拆沉及伸展时期。

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。