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Basing on detailed field survey and laboratory researches on lithological features, mineralogical composition, geochemical and zircon SHRIMP U-Pb data, together with the mineralogical study of chromitite and mantle peridotite heavy mineral bulk sample, various proceedings and recognitions have been achieved:(1) The mantle peridotite is the remnants of partial melted MOR mantle altered by SSZ fluids.

通过详细的野外调查和室内岩石薄片的岩相学、矿物成分、岩石地球化学和锆石SHRIMP U-Pb同位素年代学,铬铁矿和地幔橄榄岩的人工重砂大样的矿物学研究,取得以下进展和认识:(1)认为康金拉地幔橄榄岩为部分熔融MOR地幔残余,叠加了SSZ流体的改造。

According to the geochemical data, the formation of mantle peridotite might be: during the spreading of ocean floor, the MOR mantle underwent variable degrees of partial melting and formed the depleted mantle peridotite with podiform chromitite; during the spreading of ocean basin, intra-ocean subduction happened, REE and LILE rich fluids containing water derived from the subduction slab migrated upwards and metasomatism happened to peridotite relic.

康金拉矿区的地幔橄榄岩的地球化学特征反映了其形成过程的复杂性,表现为:洋底扩张期间,扩张脊下的MOR型地幔的经历了不同程度的部分熔融,形成了亏损地幔橄榄岩,该地幔橄榄岩中赋存了来自深部的豆荚状铬铁矿。

Therefore, it is instructive to do research on PDM using compressible fluids.

因此开展气体螺杆钻具研究工作具有重要的指导意义。

This shows that the latticeBoltzmann method can simulate compressible fluids.

这说明格子玻尔兹曼方法能够模拟可压缩流体。

Quartz is studied using an electrical conductible degree of ore-bearing fluids and infrared spectrum .

借助于成矿溶液电导度和红外光谱方法对刺猬沟和三道湾子金矿区石英进行了分析。

The quartz is studied using an electron paramagnetic resonance, infrared spectrum and the electrical conductible degree of ore-bearing fluids.

借助于电子顺磁共振、成矿溶液电导度和红外光谱方法对刺猬沟金矿区石英进行了分析。

The content of major elements, such as Fe, Mg, Ca and Al, and trace elements, such as Ti, Sr, Ni, Cr and Co, is linearly correlated to that of SiO2, which suggests that the different volcanic rocks in the basin should be the product of fractional crystallization of congenetic magmas. The parental magma may be generated by the partial melting of an enriched mantle wedge formed by the metasomatism of slab-derived fluids in an active continental margin tectonic setting.

FeO、MgO、CaO、Al2O3、TiO2等主元素和Sr、Ni、Cr、Co等微量元素的含量与SiO2含量呈明显的线性相关关系,表明该区火山岩可能是同源岩浆分异的产物,岩石形成於活动大陆边缘的构造环境,并由遭受消减板块流体交代的富集地幔楔部分熔融而形成。

Horny layer is the outmost layer of epidermis, its thickness is decided by different parts of human body, it's about 0.02mm at the thinnest parts, and 0.5mm at the thickest. It is made up of 5-10 layers of enucleated cornified cells that contains keratin and horny fat, which has the capability of resisting weak acids and weak bases , they array closely and become a natural barrier to moisture content and some chemical substances, so as to prevent the water logging of bodily fluids and endosmose of chemical substances.

角质层是表皮的最外层,其厚度依身体部位的不同而定,最薄处约0.02mm,最厚处约0.5mm由5-10层含有角蛋白和角质脂肪的无核角化细胞组成,角质层细胞有抵抗弱酸弱碱的能力,角质层细胞排列紧密,对水分及一些化学物质有天然屏障作用,因而可以阻止体内液体的水渗和化学物质的内渗。

Mitigation methods such as vacuum insulated tubing to limit heat transfer, nitrogen foam spacers to give highly compressible trapped fluids, crushable urethane foam insulation, etc. are somewhat successful, but are either very expensive, logistically troublesome or have unacceptable failure rates.

采用真空绝热油管降低热传导、利用氮气泡沫隔离液形成高压缩圈闭流体、可压碎尿烷泡沫绝热等减轻方法在一定程度上可以取得成功,但是要么费用非常高、作业麻烦,要么失败率很高。

In addition, we discuss the important role of fluids played in the generating and triggering processes of large crustal earthquakes.

并进一步探讨了流体在地震孕育及触发的过程中可能起的重要作用。

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