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.
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.
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.
结果表明，振动光谱是表征稀土氟碳酸盐矿物结构和组分特征的有效手段。
The results show that the vibrational spectra are valuable for reflecting the structure and composition characteristic of the minerals.
其中乙酸的形成有利于碳酸盐矿物的溶解，而草酸的形成不利于碳酸盐的溶解。
The formation of organic acid speeds dissolution of minerals in source rock, and the influence of the organic acid dissolving carbonate mineral influence is most obvious.
加州理工学院的科学家们说，火星上的碳酸盐矿物质是在18摄氏度左右形成的。
The Caltech scientists say carbonate minerals formed on Mars at about eighteen degrees Celsius.
烃源岩—地层水相互作用生成的有机酸促使烃源岩中矿物、特别是碳酸盐矿物溶解。
The interaction of hydrocarbon source rocks and formation water produces organic acid that can dissolve minerals, especially carbonate minerals.
分析表明，储层填隙物中的粘土矿物、碳酸盐矿物是导致该区储层敏感性的主要因素。
Shown by analysis, the main factors causing the reservoir sensibility in this area are clay minerals and carbonate.
碳酸盐岩中自生碳酸盐矿物主要为文石、高镁方解石，少量白云石、铁白云石和菱铁矿。
X-ray studies show that carbonate minerals are aragonite, high-Mg calcite, and lesser dolomite, ankerite and siderite.
成岩矿物主要为薄膜状绿泥石及加大状石英质矿物，还有自生磷灰石、充填状硅质及碳酸盐矿物。
Diagenetic minerals are mainly thin film shaped chlorite and increasing shaped quartz minerals. There are autogenous apatites, filled silicious and carbonate minerals as well.
代尼兹利有很多温泉以及石灰华。 还有很多由流水侵蚀而成的碳酸盐矿物质，成梯状，层层起伏。
The city contains hot springs and travertines, terraces of carbonate minerals left by the flowing water.
在土酸酸化反应中，盐酸不仅用来溶解碳酸盐矿物，而且具有调节氟硅、氟铝配合物平衡的另一作用；
Results have revealed that HCl can not only dissolve carbonate minerals in the reservoir but also control the equilibrium between aluminum and silicon fluoride in mud acid treatments.
喀斯特溶洞中石钟乳和石笋在形成过程中，碳酸盐矿物结晶时，常常捕获周围水溶液和气体，形成不混溶流体包裹体组合。
During the formation of stalactite and stalagmite in karst caves carbonate minerals often trap gas and aqueous fluids, forming immiscible fluid inclusion population when they are crystallizing.
风化前锋是一个重要的地球化学作用场所，在这一狭窄的界面上，伴随碳酸盐矿物的快速淋失，残余酸不溶物开始了明显分解。
The weathering front is a main place of geochemical reaction, and at this limited-thick interface, with quick dissolution of carbonates, acid-insoluble residues begin to obviously decompose.
相比之下，二氧化碳可以随岩石风化通过与硅酸盐矿物反应形成碳酸盐，直接从大气中自然收集。
In contrast, CO2 is naturally captured directly from the atmosphere by its reaction with silicate minerals to form carbonates as rocks are weathered.
相比之下，二氧化碳可以随岩石风化通过与硅酸盐矿物反应形成碳酸盐，直接从大气中自然收集。
In contrast, CO2 is naturally captured directly from the atmosphere by its reaction with silicate minerals to form carbonates as rocks are weathered.
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