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通过介绍实验条件实验方法及结果,并对其进行讨论,研究碳酸钕对A291合金组织的细化和腐蚀性能的影响。  相似文献   
3.
The plagioclase amphibolites from Kuokesu area, Kuruktag, Xinjiang occur as enclaves embedded in the granodioritic gneiss. In the light of major elements and REE data, the parent rocks of the plagioclase amphibolites belong to weak_alkaline basalts. Their Nd model ages mainly range from 2 832 to 3 075 Ma. The seven plagioclase amphibolites yield a reasonable good isochron age of (828±86) Ma(2σ) with I Nd =0.510 981±82, ε Nd ( t )=-11.5±1.6. Such a case shows the existence of great proportion of the Archaean mafic crustal basement on the Kuokesu area. The strong tectonic_thermal event at about 820 Ma made the Sm_Nd isotope of the metamorphic rocks homogenization. This event would be associated with the Tarim Movement.  相似文献   
4.
Sm-Nd isotopic characteristics, εNd(t) values and Nd model ages (TDM) of Proterozoic metasedimentary rocks in the eastern segment of Central Tianshan Belt (ESCTB), Xinjiang, are used to constrain the sedimentary provenance as well as to evaluate their tectonic implications. εNd(t) and TDM values of these samples range from -4.00 to +6.36 and from 1.29 to 2.29 Ga, respectively. These feature values are distinguished from those of Archean Tarim Craton. Their average εNd(t) values of the Weiya, the Kumishi and the south to the Dikar samples are -2.46, +2.06 and +1.37, respectively. Nd model ages of the Weiya samples vary between 1.86 and 2.29 Ga, but those of the Kumishi and the south to the Dikar samples show a significant concentration at 1.6~1.9 Ga and the youngest Nd model age is 1.29 Ga. Those Nd isotopic characteristics suggest that these metasedimentary rocks could be derived from a significant proportion of Paleoproterozoic crustal source and a participation of young arc materials, rather than Archean Tarim Craton. Furthermore, the data also indicate that these two sources were paleogeographically separated. Thus we can deduce that the Kumishi and the south to the Dikar metasedimentary rocks were formed proximal to the arc side of the back-arc basin, but the Weiya metasedimentary rocks were closer to the continental side of the back-arc basin.  相似文献   
5.
Profound geotectonic, climatic and biological changes occur during the terminal Neoproterozoic and its transition into the early Cambrian. These are reflected in temporal variations of the chemical and isotopic composition of seawater. We are studying a sequence of sedimentary rocks at the Shatan section, northern Yangtze Platform, Sichuan Province of China. This succession comprises, in ascending stratigraphic order, predominantly calcareous sediments of the Sinian upper Dengying Formation and black shales of the lower Cambrian Guojiaba Formation (time equivalent of Niutitang Fm.). Paleoenvironmental setting represents shallow-water shelf deposits. The objective of our study is to provide temporal records for the isotopic compositions of organic and carbonate carbon throughout this time interval. Organic carbon isotope values display a range between -35.8‰ and -30.1‰ with clear stratigraphic variations. Carbonate carbon isotope data vary between -3.5‰ and +0.5‰. These secular variations are interpreted to reflect perturbations of the global carbon cycle, specifically changes in the fractional burial of organic carbon. However, local conditions have further affected the isotopic signals.  相似文献   
6.
研制成用激光二极管泵浦的声光调Q的Nd:YVO4腔内倍频激光器,得到了TEM00模、频率高达100kHz的稳定的532nm绿激光脉冲系列输出,阈值泵浦功率27mW;在连续570mW的泵浦功率下,绿激光脉冲的峰值功率1.1kW,脉宽4.6ns;输出功率稳定,在±5℃的工作温度变化下,输出功率变化小于±2%。实验发现:在一定的泵浦功率范围内,随着泵浦功率的增加,1.064μm基频光的输出能量逐渐增加到一个最大值,然后又逐渐降低;而532nm倍频光的输出能量却一直单调增加;同时激光脉冲宽度也逐渐减小,趋向一个最小值;倍频光脉冲宽度远小于基频光脉冲宽度。声光调制器的质量对器件性能有很大的影响。  相似文献   
7.
汉诺坝非橄榄岩类包体的化学和同位素特征   总被引:1,自引:0,他引:1  
汉诺坝非橄榄岩包体主要是指辉石岩、辉长岩和麻粒岩,其主要元素、微量元素有较大和系统的变化,Nd、Sr、Pb同位素从非常亏损的DMM源特征变至具EMI和EMI源趋势的富化特征.它们与寄主玄武岩及共生的橄榄岩包体无直接成因联系,有不同的形成时代并在不同的空间位置居留  相似文献   
8.
Nuclear technique is a powerful scientific tool in agricultural research, an area with fruitful achievements in China. Application of nuclear technique in agriculture (Nuclear Agricultural Sciences) based on the development of related science and technology is a high-tech area, and also a significant aspect of non-electrical power application of nuclear technique. As an important component of agricultural science and technology, Nuclear technique application in agricultural field has achieved a lot and made remarkable contributions to the economic, social and ecological development of China. The current paper reviews the achievements, and presents the situation of the application of nuclear technique in the Chinese a-griculture briefly. The author strongly suggests that Chinese  相似文献   
9.
经纤支镜激光治疗原发性气管支气管淀粉样变性10例   总被引:3,自引:0,他引:3  
目的:研究经纤支镜Nd:YAG激光治疗在原发性气管支气管淀粉样变中的应用.方法:确诊原发性气管支气管淀粉样变10例,经纤支镜行Nd:YAG激光治疗.结果:4例局限性气管支气管淀粉样变成功去除腔内病灶,5例气管支气管淀粉样变伴有不同程度狭窄者管腔较前明显通畅;1例左主支气管闭塞伴左上叶不张者治疗后肺复张.结论:经纤支镜Nd:YAG激光治疗在原发性气管支气管淀粉样变性中有良好疗效。  相似文献   
10.
辽北新宾?苇子峪地区的花岗质岩石主要由英云闪长质?奥长花岗质片麻岩和二长花岗岩?正长花岗岩岩体等组成。为确定其形成年代及成因, 对这些花岗质岩石进行锆石U-Pb-Hf同位素和全岩地球化学分析。锆石LA-ICP-MS U-Pb同位素定年结果表明这些花岗质岩石均形成于新太古代, 英云闪长质和奥长花岗质片麻岩的岩浆结晶年龄分别为2588±4 Ma (MSWD=1.3)和2587±6 Ma (MSWD=1.8), 二长花岗岩?正长花岗岩则侵位于2555±4 Ma (MSWD=0.51)。全岩地球化学和锆石Lu-Hf同位素研究表明, 英云闪长质?奥长花岗质片麻岩形成于俯冲板片的部分熔融, 其原始岩浆在上升过程中受到地幔楔岩石的交代; 而二长花岗岩?正长花岗岩中一部分岩浆起源于变质杂砂岩的部分熔融, 其余形成于以变质玄武岩与变质沉积岩为主要成分的混合源区的部分熔融。结合近年的研究成果, 认为新宾?苇子峪地区的新太古代花岗质岩石可能形成于活动大陆边缘的动力学背景。  相似文献   
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