利用背面Ar+轰击改善n沟MOSFET线性区的特性

研究了利用背面Ar^ 轰击改善n沟金属－氧化物－半导体场效应晶体管（n-MOSFET)线性区的特性，用低能量（550eV)的Ar^ 轰击n-MOSFET芯片的北面，能有效地改善其线性区的直流特性，如跨导，沟道电导，阈值电压，表面有效迁移率以及低频噪声等，实验结果表明，随着轰击时间的增加，跨导，沟道电导和表面有效迁移率光增大，然后减小，阈值电压先减小，随后变大；而低频噪声在轰击后明显减小，实验证明，上述参数的变化是硅－二氧化硅界面态密度和二氧化硅中固定电荷密度在轰击后变化的结果。     

Surface modification of poly（vinyl chloride） by long-distance and direct argon RF plasma

AS AN ELECTRICALLY NEUTRAL, HIGHLY IONIZED GAS COM- POSED OF IONS, ELECTRONS, AND NEUTRAL PARTICLES, PLASMA IS A PHASE OF MATTER DISTINCT FROM SOLIDS, LIQUIDS, AND NOR- MAL GASES,KNOWN AS THE FOURTH STATE OF MATTER[1]. RECENT YEARS SEE GREAT PROGRESS IN P…     

年轻火山岩激光40Ar/39Ar定年中的n值与MSWD值

激光熔蚀⁴⁰Ar/³⁹Ar等时线法是第四纪年轻火山岩样品精细定年的新方法, 该方法处于逐步完善过程中。针对怎样判定获得的年龄结果是否可靠的问题, 通过对数据处理过程中所用参数的分析, 认为样品属性是决定年轻火山岩精细定年结果质量和可靠性的关键因素, 与样品测试数n值相关的加权均方差MSWD(mean square weighted deviation)是判断同一样品各测试点的数据是否符合正态分布, 能否用来客观地评价测试结果, 进而评估样品是否适合进行相关测试, 结果是否可靠的重要指标。其次, 属于同一真实年龄值样品的MSWD在99.7%置信区间的取值范围可通过计算加以确认, 并提出对于表面年龄和等时线年龄数据, 必须定量地考察相应的MSWD值, 判定在具有足够样品测试数(足够大的n值)的情况下, 是否符合概率统计的正态分布, 确定样品是否对应同一年龄真实值。在MSWD值达不到理想值1.0的情况下, 可以利用表面年龄概率密度曲线, 区分测试样品内部包含的非同源或非等时或封闭不好体系的数据, 再结合MSWD与n值关系, 适量地去除部分偏离正态分布的测试数据, 识别出可能归属多个年龄真实值的测试数据组, 并以此计算不同数据组的反等时线年龄, 获得年轻火山岩喷发的准确年龄。     

Behavior of argon gas release from manganese oxide minerals as revealed by <Superscript>40</Superscript>Ar/<Superscript>39</Superscript>Ar laser incremental heating analysis

Manganese oxides in association with paleo- weathering may provide significant insights into the multiple factors affecting the formation and evolution of weathering profiles, such as temperature, precipitation, and biodiversity. Laser probe step-heating analysis of supergene hollandite and cryptomelane samples collected from central Queensland, Australia, yield well-defined plateaus andconsistent isochron ages, confirming the feasibility dating very-fined supergene manganese oxides by 40Ar/39Ar technique. Two distinct structural sites hostingAr isotopes can be identified in light of their degassing behaviors obtained byincremental heating analyses. The first site, releasing its gas fraction at thelaser power 0.2-0.4 W, yields primarily 40Aratm, 38Aratm, and 36Aratm (atmospheric Ar isotopes). The second sites yield predominantly 40Ar* (radiogenic 40Ar),39ArK, and 38ArK (nucleogenic components), at ～0.5-1.0 W. There is no significant Ar gas released at the laser power higher than 1.0 W, indicating the breakdown of the tunnel sites hosting the radiogenic and nucleogenic components. The excellent match between the degassing behaviors of 40Ar*, 39ArK, and 38ArK suggests that these isotopes occupy the same crystallographic sites and that 39ArK lossfrom the tunnel site by recoil during neutron irradiation and/or bake-out procedure preceding isotopic analysis does not occur. Present investigation supports that neither the overwhelming atmospheric 40Ar nor the very-fined nature of the supergene manganese oxides poses problems in extracting meaningful weathering geochronological information by analyzing supergene manganese oxides minerals.     

空气中熔化生长Nd-Ba-Cu-O超导体的Ar气处理与相稳定性

利用X射线衍射及扫描电镜等方法，研究了Ar气处理温度对空气中熔化生长的NdBa2Cu3O7-δ＋20％Nd4Ba2Cu2O10样品超导性能和组织结构的影响。结果表明，在大气环境中放置20个月的情况下，经900℃Ar气处理的样品易碎裂，且超导性能明显降低，显示出超导相的不稳定性；在500℃下经较长时间Ar气处理的样品，起始转变温度可达93K，且结构和性能均较稳定。     

40Ar-39Ar ages of the Louzidian-Dachengzi ductile shear zone near Chifeng, Inner Mongolia and their tectonic significance

The Louzidian normal fault occurs as the eastern detachment fault of the Kalaqin metamorphic core complex. Field observations and microstructural analyses reveal that the Louzidian-Dachengzi ductile shear zone developed in its lower-plate was genetically related to sinistral strike-slips and extensional faulting. Two samples from this ductile shear zone yield ⁴⁰Ar-³⁹Ar plateau ages of 133 Ma (Bi) and 126 Ma (Kp), which are concordant with their isochron ages. The plateau age of 133 Ma (Bi) records the formation age of the ductile shear zone. The inconsistent relationship between the earlier strike-slip ductile shear zone and the later normal fault makes the Kalaqin Quasi-metamorphic core complex distinctive from Cordilleran metamorphic core complex. These ages provide important geochronological data for putting constraints on the formation age and genesis of such ductile shear zones.     

40Ar-39Ar thermochronology of two ductile shear zones from Yiwulüshan, West Liaoning Region: Age constraints on the Mesozoic tectonic events

Two ductile shear zones trending EW and NNE respectively not only controlled the tectonic framework of the northern North China, but also constrained the geodynamic background for gold mineralization in this region. Field observations and microstructural analyses reveal that the EW trending ductile shear zones are mainly contributed to dextral compressional deformation resulting from top-to-the-southeast oblique thrust shearing, whereas the NNE trending ones are genetically related to sinistral strike-slip and extensional faulting. One sample from the former yielded an ⁴⁰Ar–³⁹Ar plateau age of (219± 4) Ma (Bi) and two samples from the latter gave ⁴⁰Ar–³⁹Ar plateau ages of (116± 2) Ma (Bi) and (127±3) Ma (Bi). These ages provide constraints on the top-to-the-southeast oblique thrusting event occurring in Late Triassic and the sinistral extensional and strike-slip faulting event which occurred in Early Cretaceous.     

Potash-rich volcanic rocks and lamprophyres in western Shandong Province: 40Ar39Ar dating and source tracing

Highly precise 40Ar39Ar dating results demonstrate that the ages of potash-rich volcanic rocks in western Shandong Province are 114.7-124.3 Ma, and that of the lamprophyres is 119.6 Ma. The potash-rich volcanic rocks have relatively high (87Sr/86Sr)i ratios ( 0.708715-0.711418)and distinctly negative εNd values ( -11.47 - -17.54), and are enriched in radiogenic lead (206Pb/204pb=17.341-17.622,207pb/204Pb=15.525-15.538, 208Pb/204pb = 37.563-37.684).Similarly, the lamprophyres also have quite low εNd values ( -11.57 - -19.64). Based on the fact that the Sr, Nd and Pb isotopic compositions of potash-rich volcanic rocks are very consistent with that of the clinopyroxene separates, and by integrating comprehensive analyses of their tectonic settings,and extensive comparisons of the Sr, Nd isotopic compositions with that of the related simultaneous rocks, it is concluded that the potash-rich volcanic rocks and lamprophyres in western Shandong Province were most possibly derived from the partial melting of enriched mantle which was caused by source contamination and metasomatism of subducted continental crustal materials.``