布朗单样本轨道的重分形分析

主要研究布朗单W＝{W（s1,s2)s1，s2≥0}样本轨道的重分形分析问题．在布朗单一致连续模的基础上讨论“α—快点集”的重分形分析性质，得到了两类不同增量形式的“α—快点集”的Hausdorff维数．     

基于多重分形谱的图像索引方法研究

讨论了图像多重分形谱的计算方法及简化算法,对图像多重分形谱的一些特性进行了概括,利用简化 算法求得的多重分形谱数据对图像进行索引,给出了一些改进方案用于进一步研究。     

波阻抗反演技术在孤东地区馆陶组薄储层描述中的应用

根据一维波动方程的拟合迭代法原理 ,给出了求解波阻抗σ(x)的算法。针对孤东地区馆陶组薄储层油藏存在的地层埋深浅、较疏松以及井径变化大泥岩中含有膨化矿物蒙脱石等引起的声波测井速度失真问题 ,采用分段函数法对其进行了校正。将校正后的声波资料进行反演 ,可得到高质量的资料 ,用该校正资料追踪描述的储层与录井结果吻合较好。应用结果表明 ,测井资料在反演中可以补充地震资料缺少的低频和高频分量 ,地震波阻抗反演技术是薄储层描述的有效方法     

Emergent Property in Macromolecular Motion

In this paper, the model of inverse cascade fractal super-blocks along one direction (in the positive or negative) in the 3-dimensional space is developed to describe the self-similar motion in macromolecular system. Microscopically the cohesive and dispersed states of the motion blocks are co- existent states with vastly different probability of occurrence. Experimental results and theoretical analysis show that the microscopic cohesive state energy and dispersed state energy of each motion block are respectively equal to the macroscopic glassy state energy kTg and molten state energy kTm of the system. This singularity unveils topologically the non-integrability, mathematically the anholonomy, and macroscopically the emergent property. This singularity also reveals that the glass, viscoelastic and melt states are three distinct emergent properties of macromolecular motion from a macroscopic viewpoint. The fractal concept of excluded volume is introduced to depict the random motion at various scales in     

Present-Day crustal deformation field in China continent inverted from GPS observations, earthquake moment tensor and quaternary fault slip rates

Based on the bi-cubic Bessel spline function method, we have inverted the present-day crustal horizontal velocity field and deformation field in China continent by combining with 410 GPS observations, 327 seismic moment tensors of earthquakes and fault slip rates in China and its neighboring areas, and considered the geological and geophysical parameters at the same time. The results reveal that the crustal movement mostly takes on compression in SN-NE direction and extension in EW-NW direction in China continent. The continent is rotating southeast and takes on a clockwise rotation image from the west to the east, particularly in the southeast of Tibet and Chuan-dian area. Different blocks have different deformation in China continent. The south China, Ordos and Northeast block have good integrity.The deformation in the western part of China is obviously stronger than that in the eastern part. The strong strains are focused on the Himalaya, east Tibet,west Tian Shan and Chuandian block etc. The deformation at the joint of blocks is stronger than that within the blocks. The China continent deformation not only has the strike-slip faulting and extrusion feature but also has the crustal shortening and thickening feature.     

An iterative algorithm in potential-field inversion

1　Principle and MethodAll the problems of potential- field inversioncan be concluded that of solving nonlinear functionas follows:b =f( x) ( 1 )where x =( x1,x2 ,… .xn) T,xj( j =1 ,2 ,… ,n)indicate geometricparameters and physical parame-ters of the object;b=( b1,b2 ,… ,bm) T,bi( i=1 ,2 ,… ,m) indicate potential- field measurements.Main algorithms for expression( 1 ) are leastsquare method ( include damping least squaremethod ) ,gradient method ( conjugate gradientmethod and variable met…     

重磁电震信息联合反演的随机建模技术

为了把目前的重磁反演从理论建模延伸到随机建模领域，本文从物理场、级数理论出发提出了重磁统计推断建模反演的方法．该方法在重磁场源分离的基础上，以断裂系统把研究区划分为一些独立的次级单元．在各单元内把要反演的地下界面深度作为其对应的极值重磁异常的二元复合逆函数，利用已知的重磁电震剖面资料，统计推断其逆函数的级数分布，以建立重磁电震联合反演的随机地质模型．应用该方法获得了合肥盆地的结晶基底构造图．该项技术探索．有潜能推进综合地球物理信息勘探技术发展．     

纵横图趣谈

纵横图的研究由来已久,首先介绍n阶纵横图问题和n阶不全四角问题及其它们的解法,然后从一道竞赛题得出启示,推广n阶不全四角问题.     

应用图论求解工艺尺寸链

简要地介绍了图论理论，阐述了图论与工艺尺寸链的内在联系，并通过示例具体介绍了应用图论求解工艺尺寸链的方法。     

P-内射模的特征

引进P-内射维数的概念，给出P-内射模的一些性质，并且用P-内射维数刻划了半单环、Von Neumann正则环和遗传环的特征。