矿体

The mesothermal lode Au refers to the ore bodies that came chiefly from magmatic hydrothermal ore-forming solution, formed in middle depth environment and lied in ore veins.

以岩浆成矿热液为主，形成于中深环境，产于矿脉中的金矿体，称中深脉型金矿。

The metalliferous ore that fills a fissure in a rock formation.

在矿体的许多部位，异离体矿石表明有非常特征性的流动构造。

Our factory has rich mineral resources of silicon, Orebody disk belonging to the Late Paleozoic mud line vault Coastal Stream Group - neritic facies sedimentary deposit.

我厂拥有丰富的硅矿资源，矿体属于晚古生代泥盘系跳马涧组滨海——浅海相沉积矿床。

Sulfides with framboidal and oolitic texture have been found from massive sulfide ore.

块状矿体中发育典型的草莓状和鲕状硫化物。

And Majiahe Fm. of Xiong'er porphyritic andesite group. No gold deposits without fault structures, for gold deposits greatly dominated by regional fault.

区内断裂构造是控制金矿体分布的最主要因素，可以说没有断裂构造就没有金矿床的产出。

Studies on rock and ore micro fabric that control mineral preservation stratum of the deposit,and the siliconization and pyritization contacted with gold mine origin reflects the characteristic of syndepositiondiagenesis,which indicates the sediment-diagenesis and later stage mild reconstructive genetic mechanism of Shuiyindong gold deposit.

黔西南水银洞金矿是一特大型富金矿床，矿体成群多层、顺层产于龙潭组地层中，通过系统研究水银洞金矿赋矿地层岩石及矿石的显微组构特征，以及与金矿成因联系密切的硅化及黄铁矿化特征，均显示为同沉积—成岩特征，共同指示水银洞金矿沉积—成岩后期轻微改造的成因机制。

We calculated the Seebeck coefficient and power factor for filled-CoSb3 skutterudites, and our calculated S is in consistent with the experimental results.

研究发现了填充方钴矿体系的最佳载流子浓度为5×1020/cm3。

The mantle shear zone formed at lithospheric extensional setting of Meso-Tethys and reworked by serpentinization, cataclasis, and compressional deformation including deformed lens such as ophiolite, gabbro, and chronite, thrust faults, and folds produced during closure of the Meso-Tethys.

在南北向挤压导致海盆消亡的早期阶段，处于深层侵位环境的地幔橄榄岩由于物性的不均一性，变形分解作用产生不同尺度的透镜网络，如蛇绿岩体、辉长岩脉、纯橄岩异离体、豆荚状铬铁矿体、眼球状橄榄石、辉石残斑晶等。

From the fields of regional crust-mantle structure, metallogentic settings, history of tectonic-magmatic activity, distribution of high antimony anomaly, characteristics of deposit, origin of ore-forming materials (including Sb, C, Si, S, solution and associated elements), black dikes, the relation of deposit and mantle metasomatism fluid is expounded by means of geology and geophysics. Xikuangshan antimony deposit is proved to be a typical vein deposit formed by mantle metasomatism fluid. On the basis of this knowledge, the prospecting criteria of blind orebody of the deposit are given as follows: extensive structuer which indicating the activities of mantle metasomatism fluid, change of host rocks (especially exsisting shale barrier bed), silication and carbonization alteration.

文中对地幔交代流体组成、性质、活动特点及其成岩、成矿作用作了综述与探讨；从锡矿山区域壳幔结构和成矿背景、地质构造-岩浆活动史、高锑地球化学场结构分析、矿床特征、成矿物质(包括Sb、C、Si、S、流体及伴生元素)、与成矿有时空联系的暗色脉岩等方面入手，利用地质、地球物理、地球化学手段多方面论述了矿床与地幔交代流体活动的关系，论证了锡矿山超大型锑矿的地幔交代流体成因，并以此为基础提出盲矿体地质找矿标志：即指示地幔交代流体活动的构造，尤其是具有成矿元素和碱质异常、热液蚀变的断裂构造；有利的岩石物理化学性质；硅化、碳酸盐化围岩蚀变等。

A methodology is presented for the spatialization and regularization of geological data in developing a volume visualization system of mineral deposits.

系统地论述了矿床体视化过程中由原始采样数据生成空间规则体数据的实现方法，分析了能够形成地矿体空间体数据的主要插值方法的优缺点，在充分考虑矿石品位的空间相关性和变异性的前提下，利用Shepard法实现了空间体数据的生成

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。