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dolomite相关的网络例句

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与 dolomite 相关的网络例句 [注:此内容来源于网络,仅供参考]

INTUITION Mineral: Dolomite Dolomite is holding the vibration of intuition in the language of light.

直觉 矿石:白云石白云石持有光之语中直觉的振动。

The flotation mechanism of MG reverse-floating dolomite was studied by measuring the Zeta-potential of collophanite and dolomite, Infrared Absorptions Spectra analysing the adsorption of MG onto the minerals surface, ultraviolet- visible light absorbing spectrum calculating the amount of MG which was adsorbed onto the minerals surface. These researches showed that MG was more easyly adsorded onto the surface of dolomite in feeble acidic solution because of pure dolomite charges positive as well as pure collophanite charges negative. Therefore, a lot of MG negative ions was adsorded onto dolomite, and that MG negative ions contained hydrophobic group, the hydrophobicity of dolomite was modified, the grains of dolomite were adhered to air bubble and float with them.

对白云石和胶磷矿的Zeta-电位测定、红外光谱分析MG药剂在矿物上面的吸附情况、紫外-可见吸收光谱测定矿物上MG的吸附量等,研究了MG药剂反浮选白云石的浮选作用机理,表明在弱酸性条件下,由于白云石表面荷正电而胶磷矿表面荷负电,带有羧基和羟基官能团的MG药剂更容易吸附在白云石上,使其周围吸附有大量的MG负离子,而MG负离子的另一端为烃基,这就改变了白云石的疏水性,使其矿粒容易附着于气泡上浮。

The main sedimentary facies types include shoal facies of platform margin, organic reef facies of platform margin, platform evaporate facies, open-platform facies, restricted platform facies and carbonate platform ramp facies, and the front three types of facies are the uppermost facies belt. The main sedimentary microfacies types include subordinate organisms dolomite microfacies, sparry grain(biogenic debris, sand cutting, alga chippings and so on) dolomite microfacies, detention gravel debris dolomite microfacies, boundstone microfacies, non-lamina dolomite mudstone microfacies, lamina dolomite mudstone microfacies, lamina lime mudstone microfacies, sparry grainstone microfacies and testaceous chippings limestone microfacies, and the front three types of microfacies are the uppermost microfacies type.

该区长兴组主要的沉积相类型有台地边缘浅滩相、台地边缘生物礁相、开阔台地相、局限台地相、台地蒸发岩相和碳酸盐台地缓坡相六个相带,主要的微相类型有生物粘结云岩微相、亮晶颗粒云岩微相、滞留角砾云岩微相、纹层纯云泥岩微相、非纹层纯云泥岩微相、生物粘结灰岩微相、纹层纯灰泥岩微相、亮晶颗粒灰岩微相和介屑灰岩微相九种微相类型。

Moreover, reef-shoal dolomite (subordinate organisms and sparry grain dolomite microfacies) reservoir pores develop with a large-scale distribution, abundant dissolved pore types and excellent reservoir capability; evaporite platform dolomite (non-lamina dolomite mudstone microfacies) takes second place with average reservoir capability; reef limestone pores develop with lower reservoir capability, regarded as III class of reservoir at most; open-platform limestone (non-lamina dolomite mudstone microfacies)pores underdevelop with no reservoir capability.

此外,通过孔隙演化研究可以看出礁滩云岩(生物粘结云岩和亮晶颗粒云岩微相)储层孔隙规模最大,溶孔类型丰富,储集性能最好;蒸发台地云岩次之,储集性能一般;礁灰岩孔隙也有发育,储集性能较差;开阔台地灰岩孔隙不发育,几乎不具备储集能力。

For the first time, the RMF will organise an Open Women's Cup, and female climbers from all over the world are invited to take part. The athletes will compete on the most popular peaks of the Western Caucasus: Dalar, Dolomite and Kirpitch.

2008俄罗斯攀岩锦标赛首次设立女子项目,盛邀各国攀岩女将参赛,攀岩目标是业内最为青睐的西高加索山脉的 Dalar 、 Dolomite 及 Kirpitch地区的数座山峰。

Using methods of sedimentary and geochemistry, this paper analyzed the sedimentary environment in the Majiagou Formation. It suggests that Member 1, Member 3 and Member 5 are characterized by a dry and hot climate as well as fall of the sea level. The area of Well Longtan 1 in the eastern basin is abundant of platform evaporites with the depositional anhydrite and salt rock, surrounded by a suite of dolomite intercalated by the thin layers of anhydrite from the anhydrite\|dolomite platform sediment. It deposits muddy dolomite, dolomitic limestone and fine\|grained dolomite in the limestone-dolomite platform and restricted sea.

运用沉积学与地球化学方法,分析了研究区马家沟组的沉积环境,认为:马一段、马三段和马五段沉积时期气候干热,海平面下降,盆地东部龙探1井区一带主要为台地蒸发岩相沉积,发育了膏盐岩和盐岩沉积,其周边则发育了一套白云岩夹薄层硬石膏岩的含膏云坪相沉积,在盆地东部周边地区主要沉积了泥质白云岩、白云质灰岩和细晶白云岩的云灰坪和局限海相沉积。

Spatial distribution characteristics of dolomite sandification in the research area is inducted. Macroscopic mechanism of dolomite sandification is deeply studied. The effect of dolomite sandification to lithologic association, geological structure condition, hydrodynamic conditions of groundwater, hydrochemistry condition and so on is systematically analysed.

对研究区白云岩砂化的空间分布特征进行了归纳,并深入探讨了白云岩砂化的宏观机理,系统的分析了岩性组合、地质构造条件、地下水动力条件、水化学条件等对白云岩砂化的影响。

Namely, with respect to Changxing Formation in the region of interest, the most favorable facies belt is reef-shoal dolomite facies, the more favorable facies belt is restricted platform facies-platform evaporate facies; the most favorable microfacies belt is subordinate organisms and sparry grain dolomite microfacies, the more favorable microfacies belt is non-lamina dolomite mudstone microfacies.

因此长兴组最有利储集相带是礁滩云岩相带,较有利相带是局限台地-台地蒸发岩相带;最有利微相类型是生物粘结云岩微相和亮晶颗粒云岩微相,较有利的微相类型是非纹层纯云泥岩微相。

Based on the study of rock textures and structures, and stable isotopes of dolomite and S isotope of barite interlayers within the cap dolomite outcropped in the Miaohe area in the Three Gorge, it is testified that the stable isotopes show a strong negative excursion, and the isotopes of sulfur show a significant positive excursion, which is similar to the reported data of authigenic barites formed in a modern seafloor gas hydrate environment. Therefore, it can be concluded that the cap dolomite was most likely formed in a special environment under which a huge gas hydrate dissociated with the breakup of "Snow Earth" in later Neoproterozoic.

通过对湖北三峡庙河地区出露的&盖帽&白云岩的野外地质构造、碳-氧稳定同位素和重晶石夹层的硫稳定同位素特征的研究,发现除了明显的碳稳定同位素的负偏移之外,重晶石的硫同位素值表现出明显的正偏移,其数值可与现代海底甲烷喷气孔附近的自生重晶石矿物的同位素组成相对比,进而认为&盖帽&白云岩的成因是末元古代&雪球&事件之后天然气水合物的释放与全球环境突变背景下的沉积产物。

The experimental results show that when TCAR is about 700 ℃ XN for limestone is maximum, and the optimum TCAR for dolomite is about 650℃. Although XN for limestone is much higher than dolomite, the difference of their YN is little when TCAR is in 650~700 ℃. And if TCAL is beyond 1050 ℃ XN for limestone decays sharply, but it is negligible to dolomite. XN for dolomite is far higher than limestone in the high TCAL. XN for limestone decreases with the particle size increasing, and there is an optimum particle size range with particle size increasing which XN for dolomite reaches maximum in. The particle size plays a more important role in limestone carbonation process than dolomite.

结果表明:TCAR为700℃时石灰石的XN最高,白云石则在650℃时XN最高,在650~700℃时白云石的XN远高于石灰石,但它们的YN相差不大;当TCAL超过1050℃时石灰石的XN急剧衰减,而白云石的XN则衰减程度不大,在高温煅烧时白云石的YN比石灰石更高;随粒径的增大,石灰石的XN逐渐减小,而白云石则存在最佳的粒径分布使XN最大,粒径的变化对石灰石的XN影响更大。

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