华北克拉通恒山地区晚太古代变质火山岩的地球化学特征及构造意义

对恒山地区出露的变质火山岩开展岩相学、地球化学、锆石U-Pb年代学和Hf同位素研究,旨在确定其形成时代,探讨岩石成因及地球动力学意义。锆石U-Pb定年结果表明,这些变质火山岩喷发于新太古代晚期(2508±20Ma)。地球化学分析结果显示,恒山变质火山岩由变质玄武岩和变质玄武安山岩组成,SiO₂(45.51%～62.67%)、FeO_T (4.43%～15.72%)和MgO (3.75%～8.14%)含量变化幅度大,是幔源岩浆经单斜辉石、角闪石和磁铁矿分离结晶的产物。这些变质火山岩富集轻稀土(LREE)和大离子亲石元素(LILE),亏损重稀土(HREE)和高场强元素(HFSE),具有相对高的Th含量和Th/Yb比值,呈现钙碱性岛弧火山岩的特征。结合不相容元素比值Nb/Yb,Zr/Yb和(Nb/La)_N的特点,推测其来源于俯冲带具流体交代特征的富集地幔源区。结合区域构造背景,推断恒山变质火山岩形成于新太古晚期大陆弧环境。     

动态可控残差卷积神经网络的低剂量 CT 图像处理

针对计算机断层扫描(Computed Tomography, CT)中因采用低剂量扫描方式,导致图像噪声伪影干扰,尤其 是不同部位噪声和伪影强度存在较大差异这一问题,提出了一种基于动态可控残差的卷积神经网络(DC-ResNet) 算法。 DC-ResNet 的主要思想是在常规残差网络连接中添加一个图像质量指导的控制变量,以允许获取残差的加 权和,从而实现残差特征的动态可控。 所设计的 DC-ResNet 网络是一种包括两个子网络的组合型结构,一个是作 为主干网络的基础子网络,在该子网络中使用全局动态残差块和局部动态残差块来实现低剂量 CT 图像质量的提 高;另一个是作为辅助网络的条件子网络,用来生成基础子网络中不同动态可控残差块的权值,辅助基础子网络的 学习。 通过 Mayo 与 UIH 数据实验验证,其视觉结果表明:处理后的不同部位 CT 图像噪声伪影均能够得到较好的 抑制,并能有效地保留结构细节及组织纹理;量化结果表明:处理后的 CT 图像峰值信噪比( Peak-Signal to Noise Ratio, PSNR)和结构相似性(Structure Similarity, SSIM)均优于对比方法。     

胶东-辽东-朝鲜巨型金矿集中区的分离

胶东、辽东、朝鲜北部三区在地质上表现出了极大的相似性和稳定性。它们不但在元古代地层上可以相互对比,而且还有着一个统一的硼的地球化学省,在大地构造单元上也可以相互衔接。三区可以拼合为一个整体,使辽东的丹东金矿区、朝北的平安北道金矿区和胶东的招掖金矿区正好合成一个完整的整体,构成了一个巨大的金矿集中区。这个巨型金矿集中区是在统一的古陆块上由同一成因作用形成的,后因大陆的张裂和离散被分离。文中对它的分离机制和过程进行了探讨。     

The in vivo expression of the globin genes of theβ cistron in γ-,δ-, andδβ-thalassemia heterozygotes

There is considerable evidence suggesting that the switch from to and chain production after birth is due, in part, to silencing of the genes by stage-specific factors which bind to their promoters and to the competition from the adult ( and ) genes for a common enhancer element located in the locus control region. As a consequence one can expect that the increased Hb F production in adults with hereditary persistence of fetal hemoglobin or -thalassemia is directed mainly by -globin genes in cis to the deletion(s) responsible for these conditions. Here we review data on heterozygotes with -, -, or -thalassemia, who also had an^AT mutation, in cis or in trans, which was used as a marker of gene expression. The results show that a deletion affecting adult genes favors the expression of genes in cis, while the deletion of a single gene does not affect the expression of the gene in cis but leads to a faster switch postnatally.     

Critical slope gradient for compulsory abandonment of farmland on the hilly Loess Plateau

Scientific evidence for the upper limit of farmland is proposed. Shallow gully erosion is one of erosion types distributed extensively on sloping farmland in the hilly regions of the Loess Plateau. Field observation and aerial photos interpretation, as well as laboratory experiments show that the shallow gully erosion occurring on the steeper farmland in the hilly regions of the Loess Plateau is an important factor leading to intensive erosion on slope, because of its extensive distribution and intensive runoff collection. The data on the formation, development and distribution of shallow gullies on sloping farmland indicate that critical slope gradient for shallow gully initiation ranges from 15 to 20 degrees with an average of 18.2 degrees. Therefore, it is suggested that critical slope gradient for compulsory abandonment of farmland on the hilly Loess Plateau should be kept within the critical slope gradient for shallow gully initiation to prevent shallow gully formation in order to control soil loss more effectively. But as the first step, the cultivation on the slopes with slope larger than 25 degrees where the maximum erosion occurs should be strictly forbidden.     

保守系统的混沌同步

发现保守系统相空间中的一个轨道囚禁区．用闭环控制方法将系统引入囚禁区并在其内实现了同步．     

关于运城地区发展经济林的反思

优越的农业自然条件使运城地区成为山西省重要的粮棉生产基地。但近年来经济林的迅速发展使果树栽植面积几乎占到耕地总面积的1／4。尽管平原地区广种经济林具有一定的经济效益与环境效益,但它却违背了合理利用土地的原则,若不及早采取有力措施加以控制,我国将会潜伏粮食危机,种植业的可持续发展将会受到严重影响。     

AlGaAs／GaAs HBT基区电流的研究

在ALGaAs/GaAs HBT E-M模型直流参数的研究基础上,对HBT的基区电流进行了研究,特别是针对BE结空间电荷区的复合电流和基区表面复合电流,因为在HBT的小偏置情况下,HBT的BE结空间电荷区的复合电流和基区表面复合电流在整个基区电流中占有主导地位。当BE结间外加电压为0.5-1.2V时,ALGaAs HBT的基区电流的计算机模拟值和测试值比较接近,这一研究结果有助于进一步了解HBT的直流特性和1/?噪声特性。     

New evidence for the Qinghai-Xizang (Tibet) Plateau as a pilot region of climatic fluctuation in China

Over 40 a observed temperature data in 172 stations in China and historical proxy data were analyzed. Evidence suggested that during 1980–1994, the warmest year appeared first in southeastern part of the Qinghai-Xizang (Tibet) Plateau (henceforth SETP) and then gradually spread northwards and eastwards to eastern China. The climatic change on century time scale in recent 600 a shows 3 relatively warm and clod stages in China. Each warm and cold stage appeared first in Tibet Plateau (henceforth TP) and then in the Qilian Mountains, then in the eastern parts of China. The warm and cold stages in TP were 10–60 a earlier than in the eastern China. The facts show that TP is a pilot region of climatic fluctuation in China on the time scale shorter than 10³a.     

关于对流方程的一类三层显格式

本文对对流方程ut＝aux建立了中间层包含两个节点,带两个参变量m,k的一般三层显格式．当m,k满足一定关系时,上述格式变为二阶格式．稳定性分析表明,当参数k＜1／2时,格式的稳定条件为网格比的绝对值不超过1,这一点区别于色散方程的类似情况．