- 更多网络例句与填金的相关的网络例句 [注：此内容来源于网络，仅供参考]
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Mr. Budd told his story to an important-looking officer, who listened very politely and made him repeat the bits about the tooth which was filled with gold, the thumbnail and the hair which had been black before it was grey or red and which was now dark brown.
巴德先生把情况告诉给了一位看上去很重要的警官，警官非常有礼貌地倾听着，又让他把关键的部分再说了一遍：镶填的金牙，受损的指甲，以及原来是黑色，后来变得花白，再后来染成红色，现在已经变成深褐色的头发。
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1:250000 geological mapping has further revealed the mysteries of the tectonics of the Qinghai-Tibet Plateau. The Altun Mountains are not of the Tarim massif, but a part of the Kunlun-Qilian-Qinling orogenic system; the Altun fault is a large transform fault; the Muztag-Maqên suture zone and Jinshajiang suture zone are both Variscan ones; the Songpan-Garzê area in the Triassic was a huge turbidite basin on the southern margin of Laurasia; the Gangdise belt underwent the important Indosinian orogenic movement; an ocean basin that persisted from the Paleozoic to Triassic did not exist, i.e. the so-called Paleo-Tethys or permanent Tethys was not in existence in the Qinghai-Tibet Plateau. In the Paleozoic, most parts of China, including the Sino-Korean, Yangtze and Tarim massifs and the Qinghai-Tibet Plateau, were located in south of the main ocean basin—the Central Asian-Mongolian sea way—of the Paleo-Asia ocean, belonging to the northern margin of Gondwana. The Yarlung Zangbo and Bangong -Nujiang belts were twins in the Tethyan Ocean, which began to develop into two ocean rift belts in the Triassic. The Tethyan Ocean with the Yarlung Zangbo belt as the main ocean basin belt began to be subducted in the Late Triassic and experienced a process of pulsatory plate convergence orogeny including the Indosinian, Yanshanian and Himalayan stages.
1：25万地质填图进一步揭开了青藏高原地区大地构造的奥秘：阿尔金山是昆仑，祁连-秦岭造山系的一部分；阿尔金断裂确是一条大型转换断层；木孜塔格-玛沁缝合带和金沙江缝合带均是华力西缝合带；松潘甘孜三叠系沉积盆地是劳亚大陆南部边缘的浊积岩盆地；冈底斯带曾经历了重要的印支造山运动；不存在从古生代延续到三叠纪的大洋盆地，即不存在所谓古特提斯或永久特提斯；古生代时期，在青藏高原地区亦不存在具古生物，古地理分隔意义的大洋盆地，当时，包括中朝，扬子，塔里木以及青藏高原地区在内的中国大部分均位于古亚洲洋主洋盆——中亚-蒙古带之南，属冈瓦纳大陆结构复杂的北部边缘；雅鲁藏布江和班公湖-怒江带是特提斯洋中的孪生姊妹，它们均是从三叠纪起就发展成大洋裂谷带的；以雅鲁藏布江带为主洋盆带的特提斯洋，从三叠纪晚期开始消减，经历了印支，燕山，喜马拉雅3个阶段脉动式板块汇聚造山过程。
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C. Northcote Parkinson's cynical observation that work will expand so as to fill the time available for its completion.
帕金森的讽刺性见解：为了填满完成时间，工作将随之变大。
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The mantle metasomatism in western Shandong could be subdivided into two stages, i.e. early metasomatic event with interstitial phlogopite and late metasomatic event with orthopyroxene vein or orthopyroxene+phlogopite vein.
鲁西区地幔交代作用应有两期，即早期的填隙型金云母和晚期的斜方辉石脉或斜方辉石+金云母脉体的形成，早期交代介质为富含CO〓和H〓O的熔体，晚期交代介质为富硅质的熔体。
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Based on study of the thermoluminescent features of q uartz from vein No.505 and No.530 in Wenyu gold deposit,the value 10 000CPS for total thermoluminescent intensity and 150CPS for thermoluminescent peak strength of quartz were proposed as quantitative indicators to evaluate the auriferous f eature of quartz veins.According to this criteria,mapping of thermoluminescent intensity of quartz on limited parts of vein No.505 and vein No.530 were carried out,and conclusions that the deep parts beneath the e...
在对文峪金矿床505、530脉石英矿物热发光特征研究基础上，提出了以石英热发光总强度1000CPS，峰强150CPS为评价石英脉含金性的定量判别标志；根据上述准则，开展了505及530脉局部范围的石英热发光强度填图工作，并得出了505脉13中段及530脉10中段在现在矿体深部仍有较好成矿前景的结论，为脉型金矿床深部成矿远景评价提供了新的途径。
- 更多网络解释与填金的相关的网络解释 [注：此内容来源于网络，仅供参考]
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filled gold：填金
filled entry 填有内容的登记项 | filled gold 填金 | filled level 满带能级
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ionic crystal：离子晶体
金八聚体是八个金原子形成的原子团,而F中心是离子晶体(ionic crystal)中的阴离子(anion)空位,易於被电子填满. 金八聚体是最小的金原子簇,可以做为一氧化碳氧化为二氧化碳(CO2)过程中的异质(heterogeneous)催化剂,工作温度低达140K.