矿物的

Compaction , quartz secondary enlargement and kaolinite an aphase-infilling are main diageneses to damage pores . The solution of felspar and carbonate minerals are the chief diageneses to form sencondary pores .

压实作用，石英次生加大和高岭石的后期充填作用是使孔隙遭受破坏的主要成岩作用类型，长石和碳酸盐矿物的溶蚀作用是形成次生孔隙的主要成岩作用类型。

Compaction , quartz secondary enlargement and kaolinite an aphase infilling are main diageneses to damage pores . The solution of felspar and carbonate minerals is the chief diageneses to form sencondary pores .

压实作用，石英次生加大和高岭石的后期充填作用是使孔隙遭受破坏的主要成岩作用类型，长石和碳酸盐矿物的溶蚀作用是形成次生孔隙的主要成岩作用类型。

The dickite/Kaolinite interaction mineral is also found in this deposit.

无序的过渡矿物的存在代表了一种过渡的准稳定的环境。

Photo Gallery: Minerals Malachite from a Zambian mine seems to take the form of rounded peas.

意译：矿物的图片集。孔雀石来自赞比亚矿山似乎获得的形态的圆形的豌豆。

It is the interface mechanism and minerals is complex, involving physical chemistry and biochemistry parameters.

它与矿物的界面作用机理是复杂的，涉及物理化学的和生物化学的参数。

A discussion on abnormal phenomena of gemstones under polariscope;2. The meaning,classification of the transparency of gemstones and the factors affecting the transparency are elucidated.

宝石透明度的含义与分类宝石透明度与矿物的一样，均是指其透过可见光波的能力，主要与它们对光的吸收强弱有关，其大小可用透射系数来说明。

The addition of quebracho increased the hydrophilicity of the iron minerals, and changed their zeta potentials markedly, and improved the reverse flotation separation of quartz from specularite.

落叶松拷胶的添加能增强镜铁矿和磁铁矿表面的亲水程度，显著改变两种矿物的表面电性，从而实现石英和镜铁矿的反浮选分离。

In ore deposits on tops of the paleokarst denudationplanes,sericite is the most important carrier of gold.whereas in the ore depo-sits within the faults,pyrite is the most important carrier of gold.

不同的"卡林型"金矿床之间，由于形成的物理化学条件的差异，其主要载金矿物的种类也不相同。

The enrichment of minerals such as siderite and pyrite, which are sensitive to geochemical environment, in the transitional zone indicates that the geochemical environment is neutral-acidic and reductive and is propitious to the precipitation of uranium.

过渡带中菱铁矿(FeCO3)和黄铁矿(FeS2)等对地球化学环境敏感的矿物的富集，指示了有利于铀成矿的中性-弱酸性、还原的地球化学环境。

Little quantity of sulphur occur in forms of enclave and anhedraal,subhedral,euhedral crystal. The crystal size ranges from0.01mm to1. 00mm and little of size around 1μm.

少量呈包体形式产出，它形～半自形～自形晶，粒径在0.01mm～1mm间，极少量的在1μm这些硫化物中的硫，含量略低于其相应矿物的硫的含量。

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。