石英的

Thermometric measurements of inclusions in quartz have provided evidence for mesothermal hypothermal origin of the Baguamiao gold deposit.

同时，为八卦庙金矿的成矿提供了条件。石英中包裹体测温结果为八卦庙金矿床的中温成因提供了证据

By using an uncoated silica capillary(75um I.D,60cm of total length,and 50cm of efficient length)and 75mmol/L borax(pH 10.5)as carrier electrolyte,the derivatized isomaltooligosaccharides with a-naphymethamine,including isomaltose,panose,isomaltotriose,were sufficiently separated at the qualification of an applied voltage of 15kV and aUV detection wave-length of 214nm.

在未涂渍的石英毛细管中，以75mmol/L硼砂(pH 10.5)为运行缓冲液，在检测波长214nm、分离电压15kV下对低聚异麦芽糖主要组分的α-萘胺衍生物进行快速地分离测定。

Adsorption isotherms of propane, butane, propane and liquified petroleum gas on the quartz beads were determined respectively by means of the method of vacuum weighing , and the relationship between the isosteric adsorption enthalpy change and adsorbance was also reported.

用石英玻璃微珠模拟了HP－1，HP－20M，HP－17毛细管色谱柱内壁，用真空重量法测定了丙烷、丁烷、丙烯、液化石油气样品在3种模拟毛细管内壁表面的吸附等温线，并计算了等量吸附热随吸附量的变化关系。

In larger diameter conductors, and for secondary jacketing operations, the pre-heating can be done with either a gas flame or water-cooled quartz pre-heater tunnels.

对于直径较大的导体，和次要的外壳操作，或者用气体火焰或者用水冷式石英预热道都可以完成

Tne spilite-quartz keratophyre are thought to most probably crystallize from basic and acidic magmas contaminated by the convective circulating hot brine on seafloor.

细碧岩-石英角斑岩建造很可能为基性及酸性岩浆受对流循环的海底热卤水一定的混染作用后结晶形成。

Dapingzhang copper-polymetallic deposit hosted in spilite-quartz keratophyre formation is volcanic-hosted massive sulfide deposit, which formed during the Late Carboniferous and are contemporary with the intrusion of granodiorite-porphyry.

确定了大平掌铜多金属矿床为赋存于细碧岩-石英角斑岩中的块状硫化物矿床。矿床可能形成于晚石炭世，在时代上与花岗闪长斑岩的侵入相当。

It is indicated that source materials of type of lateritic gold deposit are rich-SiO 2 (quartz, SiO 2),rich-Fe and rich-Au ores or rocks.

分析指出，本类红土型金矿的矿源物质是高硅质(石英SiO2)、富铁质的富金矿石。

The zircon was dated by using the technique of single-zircon stepwise evaporation-deposition with a thermal ion mass spectrometry (Bernd Kober, 1986 and 1987). The zircon ages are 2.60-2.54 Ga for biotite-leptynite, 3.36-2.62 for mimatized leptite, and 3.53-3.08 Ga for quartzite from the iron formation.

用热离子质谱计双带源蒸发—沉积测定单个锆石晶体年龄的方法对弓长岭含铁建造中黑云变粒岩、混合岩化浅粒岩和石英岩中的锆石作了测定，获得了2.60—2.54 Ga，3.36—2.62 Ga和3.53—3.08 Ga等年龄数据。

Locals began mining oxidised vein material and ultimately narrow high grading mesothermal quartz-sulphide veins.

本机开始了采矿被氧化的静脉材料和最后分级mesothermal石英硫化物静脉的狭窄上流。

You see these rocks possess mylonitic texture which is characterized by relatively coarse-grained, augen-shaped feldspar and surrounding fine-grained quartz and mica. all of the minerals show oriented arrangement.

你看这些岩石都具有糜棱结构，表现为相对较粗的眼球状长石颗粒被细小的石英和云母颗粒所包绕，所有这些矿物均定向排列。

For a big chunk of credit-card losses; the number of filings (and thus charge-off rates) would be rising again, whether

年美国个人破产法的一个改动使得破产登记急速下降，而后引起了信用卡大规模的亏损。

Eph. 4:23 And that you be renewed in the spirit of your mind

弗四23 而在你们心思的灵里得以更新