The neodymium isotopic characteristic and geological significance of Kuokesu plagioclase amphibolites from the Kuruktag, Xinjiang, China

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.     

Nd isotopic characteristics of Proterozoic metasedimentary rocks and constraints on their provenance in the eastern segment of Central Tianshan Belt, Xinjiang

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.     

Isotopic evolution of the terminal Neoproterozoic and early Cambrian carbon cycle on the northern Yangtze Platform, South China

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.     

激光二极管泵浦的调 Q Nd:YVO_4绿激光器

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。     

汉诺坝非橄榄岩类包体的化学和同位素特征

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     

经纤支镜激光治疗原发性气管支气管淀粉样变性10例

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。     

辽北新宾?苇子峪地区太古宙花岗质岩石的形成年代、成因及其地质意义

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。     

LD泵浦的Nd:LuVO4被动调Q激光器

报道了一种LD泵浦的被动调QNd:LuVO4激光器,其中,Cr4 :YAG作为可饱和吸收体,KTP作为倍频晶体.在注入泵浦功率为7.4W时,得到的最大平均功率为0.88W,最高重复频率为27kHz,最窄脉宽为14ns的1.06μm基频激光输出.在泵浦功率为7W时,得到的脉冲绿光的平均功率为271mW,重复频率,脉宽,单脉冲能量和峰值功率分别为12.5kHz,28ns,21.7μJ和0.77kW.     

大直径掺钕铌酸锂晶体生长及其光学性能研究

在LiNbO3多晶料中依次掺入0.2mol%,0.5mol%和1.0mol%的钕,采用我们自主开发的计算机控制直拉法生长大直径Nd:LiNbO3晶体,测试了晶体的紫外-可见吸收光谱、荧光光谱和红外吸收光谱。由紫外-可见吸收光谱确定泵浦光波长,由荧光光谱确定激光振荡波长;采用X射线荧光光谱分析法测量了Nd:LiNbO3晶体中钕的有效分凝系数,结果是Nd:LiNbO3晶体中钕的有效分凝系数随着钕掺杂浓度的增加而减小。