碳酸盐矿物

随着富CO2热流体多次间歇性入侵导致了含铁碳酸盐矿物的反复多次溶解和沉淀、生物介壳大量溶蚀和长石铸模孔的形成以及绿泥石消失、高岭石增加等。

With the intermittent activity of hot fluid containing CC ^ , ferrous carbonate minerals dissolved and precipitate repeatedly many times .

LimestoneBuildup石灰岩的构成凝灰岩是由石灰岩所组成，它是在其周围湖水里的碳酸盐矿物沉淀的副产品。

Made of limestone , tufa forms as a byproduct of the precipitation of carbonate minerals from surrounding water .

基于碳酸盐矿物及本区浅层CO2的同位素组成对比分析，并结合浅部储层成岩作用与CO2的相互关系，认为CO2可能来自第三系钙质泥岩。

The correlation of isotopic constitution and the relations between diagenesis and CO2 indicate that CO2 mainly derived from Tertiary Ca-Mud rocks .

LaDY的氟碳酸盐矿物能够从成矿溶液中直接形成，而HoLu的则不能。

Fluor-carbonate minerals of La-Dy can be formed directly from ore-solutions , but those of Ho-Lu and Y can not .

X射线衍射结果表明：磷酸盐矿物中以胶磷矿为主、碳酸盐矿物主要以白云石为主、氧化物中以石英为主。

The consequence of X-ray diffraction indicate : the majority of phosphate is collophanite , the majority of carbonate minerals is dolomite , the majority of oxide is quartz .

白云质大理岩中碳酸盐矿物的δ13C值也可以用碳酸岩受到海水碳酸盐混染加以解释。

The δ 13C values observed in carbonate and silicate minerals can also be explained by carbonatite assimilated by oceanic carbonate .

作者还强调了成岩过程中由长石等铝硅酸盐溶解提供壳源Sr所造成的碳酸盐矿物成岩蚀变可能表现为较高的Sr含量；

This paper emphasizes the effect of the dissolution of aluminosilicate during diagenesis may provide more radiogenic strontium which would result in a high content of strontium in carbonate rocks .

金矿石中碳酸盐矿物的碳氧同位素组成显示成矿流体中的CO2很可能来自深部（岩石圈地幔甚或更深）。

Carbon and oxygen isotope composition of carbonates in gold ores indicates that CO 2 in ore forming fluids was probably derived from deep interior of the Earth ( lithospheric mantle or deeper ) .

腐蚀层细分为红色赤铜矿层、绿色碳酸盐矿物层和黄色锡石层组成，其厚度小于1mm。

Corrosion layer of bronze relics consisted of red cuprite sub-layer , green carbonate mineral sub-layer and yellow stannolite sub-layer .

其中，Cr（Ⅵ）毒性极强，对人体有致畸致癌作用。目前，利用生物和矿物材料（铝硅酸盐矿物、碳酸盐矿物和铁的氢氧化物等）去除重金属是研究者们关注的热点。

And Cr (ⅵ) is most toxic and carcinogenic to organism . Presently , it is hot topic noticed by researchers that the biology and mineral materials such as alumino-silicates minerals , carbonate minerals and iron oxyhydroxides , are utilized to remove the heavy metals .

稀土氟碳酸盐矿物的光致发光谱和吸收谱研究

Study on Visible Photoluminescence and Absorption Spectra of Rare-earth Fluoro-carbonate Minerals

几种铜碳酸盐矿物的光吸收谱研究

A study on the optical absorption spectra of some cu-carbonate minerals

热分析法在确定碳酸盐矿物类质同象方面的应用

Application of thermal analysis to the determination of isomorphism in carbonate minerals

选择性磁覆盖分离磷酸盐与碳酸盐矿物的研究

Research On Separation of Phosphate from Carbonate Ore By Selective Magnetic Coating

碳酸盐矿物净化含铬废水及其机理

Purifying Chromium Ion Wastewater with Carbonate Minerals and Its Mechanism

不少微生物都具有形成球状碳酸盐矿物的能力。

A large number of microbes can mediate the formation of carbonate spherulite .

碳酸盐矿物相沉积特征及其应用前景

Characteristics of carbonate mineral phase deposition and their application

以铁的碳酸盐矿物形式出现的铁矿。

Iron ore in the form of ferrous carbonate .

碳酸盐矿物氧同位素分馏的理论研究

Theoretical study of oxygen isotope fractionation in carbonate minerals

稀土氟碳酸盐矿物的拉曼光谱研究

A Raman Spectral Studies of Rare earth ( REE ) Fluoro carbonate Minerals

自生粘土发育的样品，不论其产状如何，都比不含粘土而富含碳酸盐矿物的层段的样品储集性能好。

The storage capacity of samples with clay is better than that with carbonates .

含锰碳酸盐矿物中碳酸锰组份的定量测定

Quantitative determination of manganese carbonate in mn-carbonate minerals

海相碳酸盐矿物的阴极发光性与其成岩蚀变的关系

Cathodoluminescence and diagenetic alteration of marine carbonate minerals

碳酸盐矿物阴极发光性的控制因素分析

Controlling factors of cathodeluminescence of carbonate minerals

对形成过程的动态跟踪研究是了解球状碳酸盐矿物形成机理的关键。

Tailing the process of carbonate spherulite formation is the key to understand the mechanism .

陆西地区火山岩中碳酸盐矿物氧碳稳定同位素特征

Characteristic of Carbonate Oxygen-Carbon Stable Isotopes in Volcanic Rocks in Luxi Area , Junggar Basin

微生物和Mg/Ca比则是影响碳酸盐矿物形成的非常重要的两个因素。

Microbes and Mg / Ca ratio are significant factors that affect the formation of carbonate .

青海湖沉积碳酸盐矿物之间氧同位素分馏的评估及其环境意义

Evaluation of Oxygen Stable isotope Fractionation among Different Carbonate Minerals in the Sediments of Lake Qinghai

铁的碳酸盐矿物的选择溶解

The Selective Dissolution of Ferro-Carbonate Minerals

根据碳酸盐矿物溶解动力学理论，又计算了泉水的化学年龄；

The chemical age of spring water is estimated from the theory of dissolution dynamics on carbonate minerals ;