龙门山南段邛西断层转折褶皱磁组构及其有限应变

龙门山南段位于四川盆地以西,其新生代构造变形特征对于认识青藏高原东缘的变形机制具有一定的指示意义。磁组构是一种灵敏的应变指示计,在变形微弱的沉积岩地区尤为适用。在龙门山南段邛西断层转折褶皱不同构造部位选取48个采样点开展磁组构研究,分析断层转折褶皱的有限应变特征及区域构造变形机制。实验结果表明,邛西地区上白垩统中主要载磁矿物为高矫顽力的赤铁矿,背斜整体应变较弱,且存在3种类型的磁组构,以沉积磁组构和初始变形磁组构为主,铅笔状磁组构少见,主要存在于靠近褶皱中段的前翼部位,说明断层转折褶皱前翼较后翼和核部应变强,且中段地层应变较其他部位更为强烈。此外,各采样点磁线理的优势方位为近南北向（N10°E）,表明邛西断层转折褶皱的形成与龙门山南段晚新生代近东西向的地壳水平缩短有关,暗示龙门山南段的最大主压应力方向在晚新生代存在转变的可能。     

节点突起影响格栅加筋性能的离散元研究

为研究筋土界面特性及节点突起对格栅加筋性能的影响,采用三维离散元方法,通过副颗粒的引入从构造上对节点处突起进行了模拟,并对含节点突起的三向土工格栅拉拔过程进行了仿真分析,系统研究了筋-土界面剪胀效应,揭示了宏观强度发展与细观组构演化的内在关联,明确了节点突起对格栅工作性能的改善。研究结果表明,傅里叶系数曲线与拉拔力曲线偏离较大,综合考虑法向接触力幅值与各向异性程度的组构演化系数更能准确反映宏观强度的发展;节点突起调整了纵肋内力分布,允许筋-土间发生较大程度的相对位移,更有助于材料性能的充分发挥。研究成果可为从细观角度优化格栅加筋性能提供参考。     

藏南硅质岩显微形貌的对比研究

微组构信息对硅质岩的成因具有重要的指示意义,笔者以藏南四个剖面的硅质岩样品为研究对象,观察其各自的显微形貌特征,借此对其成因类型进行了研究分析。     

Undrained Monotonic Response and Instability of Medium-Dense Sandy Soil

A series of undrained monotonic triaxial compression tests were performed on natural, medium-dense (relative density (RD) = 50%) Chlef sand containing 0.5% of non-plastic fines, under different confining pressures of 50 kPa, 100 kPa, and 200 kPa. This article focuses on distinctive states of the monotonic undrained response of sands, namely the critical state, the phase transformation state, the quasi-steady state, and the state of undrained instability (onset of flow liquefaction). Specimens were prepared using dry funnel pluviation and wet deposition to investigate the effect of the initial sand fabric on these states. The present data suggest that the initial fabric of the sand appears to have a significant effect on the undrained behavior in the early stages of shearing, with its influence vanishing at large strains. Wet deposition specimens demonstrate considerably larger undrained instability state strength than their dry funnel pluviation counterparts, and a unique critical state locus is reached by both dry funnel pluviation and wet deposition.