排序方式： 共有36条查询结果，搜索用时 15 毫秒
31.
琼东南盆地第四纪块体搬运体系的地震特征 总被引：6，自引：0，他引：6
第四纪以来,琼东南盆地的陆坡区域广泛发育深水块体搬运体系。深水块体搬运体系是广泛发生在外陆架/上陆坡的一种沉积物搬运机制,包括滑动、滑塌和碎屑流等重力流作用过程。利用深水3D地震资料,提取振幅和相干数据,通过地震剖面、构造图和时间切片分析,揭示块体搬运体系具有丘状外形、波状反射结构、弱振幅和连续性差的地震特征,内部整体比较杂乱,主体发育褶皱,趾部发育逆冲断层,具有塑性流体特征。结合南海构造背景分析,认为研究区第四纪沉积速率高并位于地震多发带,构成了块体搬运体系的形成条件和触发机制。 相似文献
32.
Taken fractal dimension, compact ratio, urban centroid and urban principal axis as the urban spatial characteristic indices, Tianjin city’s urban area is investigated in the last 26 years in a quantitative perspective, and its traits and changes during different periods are also analyzed. It is clear that these indices can not only scientifically and explicitly assess the urban morphology, urban direction and its changes and trends, but also uncover long-term effects of economy and urban planning on urban morphology. 相似文献
33.
冻土与结构接触面冻结强度研究现状与展望 总被引：3，自引：3，他引：0
全面掌握冻土与结构接触面冻结强度研究进展,是进一步深入开展冻土与结构接触面冻结强度研究的前提。首先,从接触面冻结强度定义、接触面冻结强度剪切试验仪器研发、动静荷载作用下接触面冻结强度试验、接触面冻结强度数值模拟等多个角度系统归纳接触面冻结强度方面的最新研究成果。其次,通过对比不同接触面冻结强度剪切仪,指出现有试验仪器的不足,提出接触面冻结强度成因及破坏机理缺乏深入揭示的原因,讨论现有冻土与结构接触面单元模型、接触面冻结强度预测方法等方面存在的问题。最后,提出研发改进冻土接触面冻结强度试验仪器以更好模拟实际工况的展望,指出应当运用冻土微观结构研究手段深入揭示接触面冻结强度成因及破坏机理,建议结合试验和理论推导构建更为合理的冻土与结构接触面单元模型,阐述以多影响因素试验为基础探寻更为完善的接触面冻结强度预测方法。通过国内外研究现状、存在问题及其发展趋势分析,为冻土与结构接触面冻结强度研究以及冻土区地下工程设计和隧道工程人工冻结加固等方面提供参考和指导。 相似文献
34.
将地震与测井技术相结合,对已经进入油气开发阶段、有一定测井资料的地区,提出了地震属性约束测井插值预测碳酸盐岩储层白云石体积含量平面分布的方法。方法分三个步骤:(1)利用多矿物模型测井解释技术,计算得到单井白云石含量;(2)利用地震属性与测井白云石含量曲线进行相关分析,找出相关性最好的地震属性;(3)利用Petrel软件的Convergent插值算法,在相关性最好的地震属性约束下,进行井间测井插值。该方法在川东北C地区进行了预测应用,效果较好。准确计算单井白云石含量和优选最相关地震属性,是该方法的关键。 相似文献
35.
A rapid, sensitive and reproducible high performance liquid chromatography (HPLC) method with post-column fluorescence derivatization has been developed to determine the amount of low-molecular-weight sulfated polysaccharide (GFS) in vivo. The metabolism of GFS has been shown to fit a two component model following its administration by intravenous injection, and its pharmacokinetic parameters were determined to be as follows: half-time of distribution phase (t 1/2α)=11.24±2.93 min, half-time of elimination phase (t 1/2β)=98.20±25.78 min, maximum concentration (C max)=110.53 μg/mL and peak time (T max)=5 min. The pharmacokinetic behavior of GFS was also investigated following intragastric administration. However, the concentration of GFS found in serum was too low for detection, and GFS could only be detected for up to 2 h after intragastric administration (200 mg/kg body weight). Thus, the bioavailability of GFS was low following intragastric administration because of the metabolism of GFS. In conclusion, HPLC with postcolumn derivatization could be used for quantitative microanalysis and pharmacokinetic studies to determine the presence of polysaccharides in the serum following intravenous injection. 相似文献
36.
Yintao Lu Xiwu Luan Boqing Shi Weimin Ran Fuliang Lü Xiujuan Wang Quanbin Cao Xiaoyong Xu Hui Sun Genshun Yao 《海洋学报(英文版)》2021,40(2):81-94
Analysis of 3 D seismic data and well log data from the Rovuma Basin in East Africa reveals the presence of a late Eocene channel-lobe complex on its slope. The first two channels, denoted as channel-1 and channel-2, are initiated within a topographic low on the slope but come to a premature end when they are blocked by a topographic high in the northwest region of the basin. New channels migrate southeastward from channel-1 to channel-6 due to the region's sufficient sediment supply and stripping caused by bottom currents. The primary factors controlling the development of the channel complex include its initial paleo-topographic of seafloor, the property of gravity flows, the direction of the bottom current, and the stacking and expansion of its levees. The transition zone from channel to lobe can also be clearly identified from seismic sections by its pond-shaped structure. At a certain point, thest systems record a transiton from erosive features to sedimentary features, and record a transition from a confined environment to an open environment. Channels and lobes can be differentiated by their morphologies: thick slump-debris flows are partly developed under channel sand sheets,whereas these slump-debris flows are not very well developed in lobes. Well log responses also record different characteristics between channels and lobes. The interpreted shale volume throughout the main channel records a box-shaped curve, thereby implying that confined channel complexes record high energy currents and abundant sand supply, whereas the interpreted shale volume throughout the lobe records an upward-fining shape curve,thereby indicating the presence of a reduced-energy current in a relatively open environment. Within the Rovuma Basin of East Africa, the average width of the Rovuma shelf is less than 10 km, the width of the slope is only approximately 40 km, and the slope gradient is 2°–4°. Due to this steep slope gradient, the sand-rich top sheet within the channel also likely contributes to the straight feature of the channel system. It is currently unclear whether the bottom current has any effect on its sinuosity. 相似文献