矿

The study of fluid inclusions in sphalerites and associated gangue minerals (quartz, celestite, calcite and gypsum) shows that homogenization temperatures cluster around 110-150℃, with salinities of 1.6-18.0 wt% NaCl equivalent. The fluid temperature increased with the decrease in salinities during the main ore stages, and there is also a systematic westward decrease in temperature and increase in salinity in the Jinding ore district.

闪锌矿及相关脉石矿物（石英、天青石、方解石、石膏）中流体包裹体观测的均一温度主体在110~150℃，盐度在1.6%~18.0% NaCl；在时间上，大规模成矿主要阶段伴随着流体温度的不断升高和盐度的逐渐降低；在空间上，金顶矿区空间上从东到西，成矿流体温度明显降低，盐度系统性升高。

bmsc can well adhere to and proliferate on the cementum slices and they can form a new type of mineralized tissue.

骨髓基质细胞能在牙骨质片上附着生长并形成新生矿化组织，是理想的牙周组织工程种子细胞。

Cementum is an important mineralized tissue in root formation, however , the precise mechanism of cementum formation remains undetermined.

牙骨质是牙根形成的重要矿化组织，然而，对牙骨质形成机制仍不十分明确。

Of Rare Earth of China is in Baotou , which containing 50% cerium oxide, and most of them are products as raw materials, resulting in a serious backlog.

中国的稀土80％在包头，包头稀土矿中含50％氧化铈，基本都是原料型产品，因而出现严重积压。

Made from certified organic milk,whey dominant

产物采用认证有机鲜奶、乳清蛋白为主并包含健康宝宝逐日必须的维生素和矿事物。

Products on the sulphurized surfaces of cerussite and smithsonite have been studied by means of infrared spectra,Auger electronic spectra,X-ray pho- toelectron spectroscopy and X-ray diffraction techniques etc.

本研究采用红外光谱、俄歇电子能谱、X 射线光电子能谱、X 射线衍射等手段测定了白铅矿、菱锌矿硫化表面产物。

Most of them are highly silicified and sometimes mineralized with pyrite and chalcopyrite.

大部分的扭折条带遭受强烈的硅化作用，有时还具有矿化现象，并含黄铁矿和黄铜矿。

At the same time, in the pyrrhotite around the mutative chalcopyrite, the contents of Cu increased.

结论自然铜炮制前后矿相学的变化与其成分溶出存在一定的相关性。

Taking chalcopyrite from Western Mining of China for studying object, through comparative test with and without microorganism ferribacteriales T.

采用微生物浸矿技术，以西部矿业黄铜矿为对象，进行了从黄铜矿中提取铜的实验研究。

The minerals are likely to be from the suite pyrite chalcopyrite, sphalerite, galena, fluorite and barite, and to be deposited at temperatures of between 50 and 250℃.

这些矿物可能由黄铁矿，黄铜矿，闪锌矿，方铅矿，萤石和重晶石组成，并且可能是在50～250℃之间的温度下沉积出来的。

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。