运用群状结构法求非线性波方程的函数分离变量解

随着线性物理的飞速发展,反映改变自然现象的非线性现象引起人们极大的关注,分离变量法对于求解非线性偏微分方程的初值问题是一种简单而重要的方法.分离变量解对于描述非线性现象的特征起了重要作用.本文将求非线性波方程utt=(A(x)D(u)ux)x B(x)Q(u),Ax≠0分离变量解.运用群状结构法求非线性波方程的分离变量解.给出非线性波方程的分离变量解.此方法是对方程utt=(D(u)ux)x B(x)Q(u)的推广.     

用层控矿床理论浅析白云鄂博铁矿的成矿

本文用现代成矿理论的层控矿床构造浅析白云鄂博稀土-铁矿的成矿机理,从矿床物质来源,构造成矿各个方面对矿床形成进行说明,从而对其成矿模式加以总结为“沉积变质-热液交代叠加”类型,为白云鄂博外围找矿打下基础。     

浅谈钢筋混凝土水池设计

本文从结构专业的角度,论述了对钢筋混凝土水池中所涉及的结构构造措施、伸缩缝的设置、防止裂缝延伸的措施等问题。     

浅谈异形柱框架的设计与构造

本文分析了的特点和结构布置,以及结构计算和截面选择等设计计算问题。     

浅谈地质流体及成矿作用的研究

地质流体是一定地质作用的产物,而矿床的形成过程与特定地质构造背景下地质流体的产生、运移和聚集有着密切联系。不同成矿流体的成矿机制各有差异。岩浆热液因温度降低、压力减小等因素使热液中成矿物质达到过饱和,从而产生矿质沉淀;沉积盆地含矿热卤水流体在热对流、沉积压实等作用下运移、充填、聚集;与海底基性火山活动有关的现代大洋海底热液形成硫化物矿床;地幔流体的碱交代作用形成大型-超大型中高温热液矿床。在具体的成矿过程中,各种构造环境又对流体中的成矿元素的分配、集中起到至关重要的控制作用。     

纳米晶铜中离子注入碳后的组织结构研究

对纯铜进行表面机械研磨处理（SMAT）,获得纳米晶表层,且晶粒尺寸沿深度方向逐渐增大。采用离子注入技术在纳米晶纯铜中注入碳,利用透射电子显微镜（TEM）与高分辨电子显微镜（HRTEM）进行原位动态观察。结果表明,碳在基体的表面析出,形成无定形碳膜,在电子束的照射下形成洋葱状富勒烯。同时讨论了离子注入、电子束照射、纳米晶结构及碳原子与铜原子的相互作用对碳洋葱状富勒烯形成的影响。     

Constraint on the late Mesozoic regional angular unconformity in West Liaoning--North Hebei by LA-ICP-MS dating

The angular unconformity between the Tuchengzi Formation and the Zhangjiakou Formation in the Chengde area is commonly regarded as the direct evidence of boundary between Jurassic and Cretaceous systems, and as the evidence of tectonic transformation interfaces in Mesozoic Era in the West Liaoning-North Hebei. Moreover, the lower boundary age of the Zhangjiakou Formation in the Chengde was to be thought about 135 Myr in the past. Based on the detailed study and systematic sampling in Yixian-Beipiao, Lingy- uan, Chengde and Luanping areas in the field, the authors obtained the following isotopic ages by means of LA-ICP-MS dating： In the Lingyuan area, the Zhangjiakou Formation and the Yixian Formation are in angular unconformable contact; the age range of the Zhangjiakou Formation volcanic rock is from 133 to 130 Myr （seven samples）, and that of the Yixian Formation volcanic rock is from 126 to 121 Myr （eleven samples）. In the Luotuoshan of Chengde, the Tuchengzi Formation and the Zhangjiakou Formation are in angu- lar unconformable contact; the age at the lower Zhangjiakou Formation is about 124 Myr （one sample）, which reflects that the age range of the lower Zhangjiakou Formation is from 129 to 124 Myr combined with the previous study. In the Luanping basin, there is the larg- est sediment gap in upper Mesozoic, whose lower boundary age is confined in 131 to 130 Myr. In the Yixian-Beipiao area, the second Member of the Yixian Formation, making up more than 3/4 thickness of the Yixian Formation, was formed in 126 to 119 Myr, and the age of the Yixian Formation at the bottom is about 132 Myr. Moreover, the upper boundary age of the Tuchengzi Formation is about 136 Myr in the West Liaoning-North Hebei region. Based on the above isotopic data combined with the geological characteristics in the field in the West Liaoning-North Hebei region, it reflects that there was a widespread tectonic event in the period of 136 to 126 Myr （mainly in 130-126 Myr） in the West Liaoning-North Hebei, and it formed th     

阿基米德Copula生成元的复合构造研究

本文提出了基于生成元与一般函数复合构造阿基米德Copula生成元的一种新方法．给出了二维阿基米德Copula左右复合构造的充分必要条件;对一般多维情形,给出了复合构造的充分条件;而且还讨论了左右复合构造以及复合构造与其他方法之间的联系．     

一类特殊p-群自同构群的结构

设G是p5阶有限群,对于群G具有一个循环极大子群,给出了它们所有互不同构的类型;利用半直积和全形的概念,得到了具有循环极大子群的p5阶群的自同构群的构造,同时也验证了具有这样性质的群是LA-群.所应用的方法可以用于解决所有具有循环极大子群的有限p-群及自同构群的构造.     

龙门山巨型滑覆型飞来峰体系与龙门山构造活动性

广泛分布于龙门山推覆构造带前缘的飞来蜂群构成规模巨大的飞来蜂体系,其平面展布和构造线方向与龙门山推覆构造一致,但构造倒向与龙门山推覆构造相反.其明显构造特征表明为滑覆作用形成,并且与龙门山构造演化密切相关,主要形成于喜马拉雅期.龙门山收缩变形的继续发展对飞来峰产生叠加变形,中央断裂可截覆飞来蜂,反映了龙门山构造带具有很强的新构造活动性.