一种提高地震勘探解释精度、分辨率的新方法-DDM方法

DDM(Depth—Density Method)方法是将地震时间剖面直接反演成深度、密度剖面的一种地震资料处理方法，在几千米的勘探深度范围内，该方法可以使地震勘探的精度由相对精度用绝对精度来表示；使分辨率由十几米提高到2～3米；从深度、密度剖面中，地质人员可以解释出地层的岩性，时代、砂体的厚度、沉积旋回、沉积粒序，几米、十几米的断层和褶皱，本文主要简介该方法的工作原理、地质解释的原则和在生产中的应用实例。     

聚合物后续水驱阶段剩余油挖潜技术

后续水驱阶段是聚合物驱的一个重要阶段，加强剩余油分布的研究，找准潜力所在，以便制定相应调整对策，控制含水上升速度，发挥后续水驱阶段聚合物的增油作用。通过分析该区块的地质及开发特点，发现聚合物驱后剩余油分布在断层遮挡区域、前缘席状砂相、井网不完善区域、中低渗透层段。提出了对高渗透层进行深度调剖、对窜流层进行封堵、及时进行细分注水和合理调整注采比、在剩拿油富集区布新井和过路井补孔等针对性的挖潜措施，现场实施效果良好。     

同步耦合断裂及其动力学依据

通过对地球自转速率变化推动构造运动的可能性以及地球自转角速度变化的原因和依据的讨论，提出地球自转惯性力差是决定板块相对运动趋势的主要动力学因素之一，揭示了加速期和减速期经、纬向构造之间的分布规律性，认为经、纬向构造之间的耦合关系是一种客观存在，同步耦合断裂就是由地球自转速率变化所反映的动力学状态决定的。同时，笔者对同步耦合断裂概念及耦合区构造组合的研究意义进行了探讨。     

地下排水与观测廊道加固方案的现场试验论证

华东天荒坪抽水蓄能电站上水库库底的地下排水与观测廊道为城门洞型,拱体为预制混凝土,边墙与底板现浇。运行期间发现廊道拱顶沿纵向开裂。电厂曾采用外加钢结构支撑混凝土拱顶的方案进行了加固处理,但裂缝开裂并没有得到有效控制。为弄清拱顶开裂原因,提出有效的改造加固方案,为此,进行了现场试验,结果表明:预制混凝土拱脚相对现浇边墙发生向外侧的滑动,是导致开裂的主要原因,因此,阻止其相对滑动,是加固处理的关键。     

Multidimensional Self-Affine Distribution with Application in Geochemistry

In this paper, we present the conception of the multidimensional self-affine distribution and show that the multidimensional self-affine distribution possesses the fractal property of scale-invariance under truncation, which means that theoretical study of fractals has expanded from univariate cases to multivariate cases. Application of the multidimensional self-affine distribution is illustrated by means of geochemical Au and Ag elements data sets. The fractal dimension is a parameter which can quantitatively explain the variation of geochemical elements data on some orientation. This method is applied to Au data and Ag data, but also suited for other geochemical elements data or geological data. Theory of multivariate fractal can be applied for the study of change courses of fractal system, that is, fractal dynamics.     

基于C/S模式下的用电营配管理信息系统的开发及应用

简述了以ORACLE数据库为后台数据库、VB6为编程工具的用电营配管理信息多媒体查询系统的一些技术概念，介绍了C／S模式和方法，以便更好地阐述用电营配管理信息查询系统是如何通过多媒体技术来实现的。     

单视SAR图像相干斑回波的特征分析与统计

高分辨率合成孔径雷达的相干斑是由雷达信号的干性引起的，并存在于所有相干图像中。根据SAR成橡机理，分析了产生的原因特征，给出了SAR相干斑的确切定义、统计方法。实验表明统计结果与传统方法相比更加精确。     

Far from Being "Home Alone": The Dynamics of Accompanied Fieldwork

Despite persistent images to the contrary, most fieldworkers are accompanied. Yet, there has been limited discussion on the nature of accompanied fieldwork, particularly by geographers. Drawing on our experiences in three countries in the tropics, we discuss the dynamics of being accompanied in “the field” by our children and female co‐researchers. Specifically, we focus on issues of access and rapport; the impacts of their presence on our positionality; and the implications these have for power relations and research outcomes. We demonstrate how being accompanied entangles our personal and professional selves and can result in more egalitarian power relations as we become “observers observed”. We argue that by paying attention to the dynamics of accompanied fieldwork, there is the potential to enhance the conceptual focus of our methodological concerns and to provide a more theoretically sophisticated mode of exploring the ways in which our multiple identities intersect while in “the field”.     

SEDIMENT TRANSPORT AND STREAM POWER

1 INTRODUCTION There are three basic energy dissipation rate approaches used for the derivation of sediment transport functions. They are the gravitational power theory by Velikanov (1954), the stream power theory by Bagnold (1966), and the unit stream power theory by Yang (1973, 1979, 1984, and 1986). The theoretical basis of these approaches has been summarized by Yang (1996) in his book, Sediment Transport Theory and Practice. Yang also made comparisons of the three basic approa…     

DEVELOPMENT AND APPLICATION OF AN EFFICIENT METHOD TO RIVER DISCHARGE MEASUREMENT

1 INTRODUCTION There are 129 rivers in Taiwan. Most of them are short and steep with small drainage basins and rapid flows. Heavy rains and flood flows usually carry large amount of sediment. The specific peak discharge (peak discharge per unit drainage area) in Taiwan has the highest value in the world. For example, the specific peak discharge of Wu River in central Taiwan is 10.5 cms/km2, which is about 618 times that of Yangtze River in China and 35 times that of Sinno River i…