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

直覺(jué) 礦石：白云石白云石持有光之語(yǔ)中直覺(jué)的振動(dòng)。

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.

對(duì)白云石和膠磷礦的Zeta-電位測(cè)定在线视频se、紅外光譜分析MG藥劑在礦物上面的吸附情況、紫外-可見(jiàn)吸收光譜測(cè)定礦物上MG的吸附量等2020国产一区，研究了MG藥劑反浮選白云石的浮選作用機(jī)理爱趣视频改成啥了，表明在弱酸性條件下日韩欧美日逼视频，由于白云石表面荷正電而膠磷礦表面荷負(fù)電国产三级一区二区三区在线视频，帶有羧基和羥基官能團(tuán)的MG藥劑更容易吸附在白云石上性色一区，使其周?chē)接写罅康腗G負(fù)離子，而MG負(fù)離子的另一端為烴基最新免费在线黄色网址，這就改變了白云石的疏水性1024免费手机视频，使其礦粒容易附著于氣泡上浮。

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.

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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.

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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俄羅斯攀巖錦標(biāo)賽首次設(shè)立女子項(xiàng)目人妖色偷偷福利网站，盛邀各國(guó)攀巖女將參賽久久亚洲一区二区三区明星换脸，攀巖目標(biāo)是業(yè)內(nèi)最為青睞的西高加索山脈的 Dalar 日本爱爱网站、 Dolomite 及 Kirpitch地區(qū)的數(shù)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.

運(yùn)用沉積學(xué)與地球化學(xué)方法，分析了研究區(qū)馬家溝組的沉積環(huán)境殴美真人操逼免费看，認(rèn)為：馬一段、馬三段和馬五段沉積時(shí)期氣候干熱蜜桃视频午夜播放网站免费观看大全，海平面下降A片197com网址，盆地東部龍?zhí)?井區(qū)一帶主要為臺(tái)地蒸發(fā)巖相沉積，發(fā)育了膏鹽巖和鹽巖沉積欧美视频一区久久黑，其周邊則發(fā)育了一套白云巖夾薄層硬石膏巖的含膏云坪相沉積，在盆地東部周邊地區(qū)主要沉積了泥質(zhì)白云巖2021国产在线小视频91、白云質(zhì)灰?guī)r和細(xì)晶白云巖的云灰坪和局限海相沉積欧美黄色性爱视频第一页。

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.

對(duì)研究區(qū)白云巖砂化的空間分布特征進(jìn)行了歸納污黄色深夜免费网站，并深入探討了白云巖砂化的宏觀機(jī)理黄色有限公司的网站在线进入，系統(tǒng)的分析了巖性組合99国产精品黄网站、地質(zhì)構(gòu)造條件欧美性猛交XXXXX按摩欧美、地下水動(dòng)力條件AV天堂综合网、水化學(xué)條件等對(duì)白云巖砂化的影響在线观看黄色的网站。

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.

因此長(zhǎng)興組最有利儲(chǔ)集相帶是礁灘云巖相帶，較有利相帶是局限臺(tái)地-臺(tái)地蒸發(fā)巖相帶超碰免；最有利微相類(lèi)型是生物粘結(jié)云巖微相和亮晶顆粒云巖微相91欧美在线视频，較有利的微相類(lèi)型是非紋層純?cè)颇鄮r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.

通過(guò)對(duì)湖北三峽廟河地區(qū)出露的&蓋帽&白云巖的野外地質(zhì)構(gòu)造两个小姨子木瓜电影网、碳－氧穩(wěn)定同位素和重晶石夾層的硫穩(wěn)定同位素特征的研究，發(fā)現(xiàn)除了明顯的碳穩(wěn)定同位素的負(fù)偏移之外亚洲欧美日韩黄频大全，重晶石的硫同位素值表現(xiàn)出明顯的正偏移国产欧美日韩在线综合网，其數(shù)值可與現(xiàn)代海底甲烷噴氣孔附近的自生重晶石礦物的同位素組成相對(duì)比欧美综合第128页，進(jìn)而認(rèn)為&蓋帽&白云巖的成因是末元古代&雪球&事件之后天然氣水合物的釋放與全球環(huán)境突變背景下的沉積產(chǎn)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.

結(jié)果表明：TCAR為700℃時(shí)石灰石的XN最高欧美精品网一区二区，白云石則在650℃時(shí)XN最高免费A级毛片全免费还看，在650～700℃時(shí)白云石的XN遠(yuǎn)高于石灰石，但它們的YN相差不大97超碰,人摸人人人澡人人；當(dāng)TCAL超過(guò)1050℃時(shí)石灰石的XN急劇衰減，而白云石的XN則衰減程度不大天天夜碰日日摸日日澡，在高溫煅燒時(shí)白云石的YN比石灰石更高黄色电影禁止18国产；隨粒徑的增大，石灰石的XN逐漸減小亚洲自偷自偷偷色无码中文，而白云石則存在最佳的粒徑分布使XN最大新国模吧，粒徑的變化對(duì)石灰石的XN影響更大这里只精品视频。