龙门山彭灌地区大鱼洞-九甸坪-龙溪滑覆体的变形特征及形成

论述了彭灌地区大鱼洞—九甸坪—龙溪滑覆体的构造变形特征，将其划分为南北两个滑覆体，二者以侧向镶嵌方式相连。北段为滑褶式，由两个呈上叠方式的次级滑覆体组成；南段为滑片式。滑覆体是在挤压推覆构造的后期具松弛性质的地球动力学环境下形成的，其来源于映秀—北川断裂东侧地区。滑覆活动于印支晚期至早燕山期。     

关节软骨力学行为的数值模拟

关节软骨为一由骨胶原和蛋白聚糖固体相和孔隙流体相组成的多孔材料，其可以用基于混合物理论的两相多孔介质模型准确描述。作者采用有限元数值方法分析关节软骨图限压缩蠕变和应力松弛问题，得到软骨组织在蠕变和应力松弛过程中，固体相和流体相的速度、固体相的有效应力以及孔隙压力等随时间的变化规律。所得到的结果可以为人工软骨材料和人工关节的研制提供理论参考，对生物机械工程等领域的研究具有指导意义。     

固态焊接中的等效压缩变形及应力应变分析

对固态压接升温、保温过程中存在的等效压缩变形现象及其产生进行了阐述，并在试验基础上对伴随等效压缩变形的应力应变进行了分析。结果表明：等效塑性压缩变形是焊件在升温、保温过程中受约束压力作用不能胀大而产生的塑性变形的累积，它提供了形成固态焊接接头所必需的塑性变形。等效压缩变形使焊件在被约束方向上的尺寸保持恒定，而约束压力则在焊件由表及里温升的差异、屈服极限随温度变化的不均匀性以及应力松弛的综合作用下发生增大、持平、快速减小直至缓慢减小的变化。     

Progress in the study of tectophysicochemistry

Tectophysicochemistry is a research area that deals with the interrelations between physical and chemical changes of crustal materials caused by tectonism. A given tectonic force may be resolved into two parts: homogeneous stress and differential stress. Homogeneous stress refers to isotopic pressure, which is superimposed on the original pressure and affects the equilibrium of various chemical reactions. It is also a factor that influences petrogenesis,metallogenesis and metamorphism. Differential stress is commonly produced when external forces act on a given solid body. It may cause deformation of crustal materials and generate various kinds of structural features. Tectophysicochemistry pays special attention to pressure, temperature and other physicochemical conditions produced or induced by tectonism and studies the influences of additional tectonic parameters on various chemical equilibria, so it gradually develops into an independent area of science.     

东营凹陷沙三段-沙二下亚段T-R层序特征及成因

将东营凹陷古近系沙三段沙二下亚段划分为 3个三级层序 ,即沙三下层序 (SSⅠ )、沙三中层序 (SSⅡ )和沙三上沙二下层序 (SSⅢ )。SSⅠ和SSⅡ层序由湖进体系域和湖退体系域组成T R旋回 ,其特征是代表层序边界的不整合分布局限 ,湖进体系域厚度小 ,主要为细粒沉积物 ,退积式叠加 ;湖退体系域较厚 ,由进积式叠加的砂岩、砾岩和泥岩组成。T R层序的形成主要是由于层序形成早期的构造沉降和气候起主导作用 ,其基底快速沉降 ,湖水供应充分 ,湖平面快速上升。在层序形成晚期 ,沉积物供给和气候起主导作用 ,沉积物供给多 ,快速向前推进 ,湖平面下降。构造沉降和沉积物供给因素对层序控制作用的转换促使其形成层序和体系域的边界。T R层序与三分层序之间的转换是由于层序形成的不同阶段的主控因素不同而引起的     

水力压裂中多裂缝间相互干扰力学分析

将复变函数理论与位错理论相结合 ,在考虑了裂缝表面有流体压力作用且裂缝间存在相互干扰的情况下 ,建立了无限大介质中裂尖应力强度因子的数学模型 ,利用该模型可对水力压裂中多裂缝间的相互干扰进行力学分析。假设裂缝沿着垂直于局部最大周向拉应力方向扩展 ,应用数值方法对所建立的数学模型求解 ,得到裂尖的应力强度因子及转角。数值计算结果表明 ,裂缝间存在相互干扰时所产生的剪切应力强度因子远远小于法向应力强度因子。当两个裂缝尖端垂向距离为零时 ,法向应力强度因子达到最大值。两个裂缝尖端没交叠之前裂缝基本沿着轴线扩展 ;当尖端交叠面积较小时 ,两裂尖偏离自己的轴线向避开对方的方向扩展 ;当尖端交叠面积较大时 ,两裂缝向靠拢对方的方向扩展 ,最终将贯通在一起     

边界单元法三维应力分析计算程序

以三维弹性力学问题的基本解 (Kelvin解 )为基础开发了边界单元法三维弹性应力分析计算程序 ,并对其进行了验证。结果表明 ,该程序可用来求解三维弹性应力问题 ,尤其适用于三维应力集中问题。程序中采用动态分配内存 ,自动选点积分 ,并利用分块解法求解方程组 ,有效地节省了计算机资源 ,扩大了求解问题的规模。     

Shakedown Analysis of 3-D Structures Using the Boundary Element Method Based on the Static Theorem

The static shakedown theorem was reformulated for the boundary element method (BEM) rather than the finite element method with Melan‘s theorem, then used to develop a numerical solution procedure for shakedown analysis. The self-equilibrium stress field was constructed by a linear combination of several basis self-equilibrium stress fields with undetermined parameters. These basis self-equilibrium stress fields were expressed as elastic responses of the body to imposed permanent strains obtained using a 3-D BEM elastic-plastic incremental analysis. The lower bound for the shakedown load was obtained from a series of nonlinear mathematical programming problems solved using the Complex method. Numerical examples verified the precision of the present method.     

舟桥丙丁接头接触分析的计算机模拟

深入考察接触行为的特点，并以舟桥纵向连接件丙丁接头为例，建立了两种接触计算模型。采用大型通用有限元程序进行分析，模拟丙丁接头受力时的应力应变。与经验合成计算结果和常规有限元分析的结果进行对比，证明接触分析方法对连接件塑性变形、疲劳分析和优化设计有重要的指导意义。     

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.