小波变换在东北地震趋势分析中的应用

本文在多年对东北地震大形势研究基础上,根据1900年以来东北地区地震目录资料,按年最大震级、地震频度和地震活动度分别建立三个时间序列f(t),利用离散小波变换对其进行分解,结果发现三个序列的小波变换细节系数均显示平均约20年周期的时序特征,并与该区地震活跃期符合得较好。依此,对该区地震活动发展趋势作了预测,认为当前地震活跃期大约在2008年结束。     

δ~(18)O record and temperature change over the past 100 years in ice cores on the Tibetan Plateau

1 IntroductionMeteorological stations on the Tibetan Plateau are few in number and uneven in distribution, with a majority concentrated in the east and south. No stations exist so far within the large expanse in the middle or west of the Plateau. Moreover…     

利用Surfer实现剖面平面图绘制

提出了利用Surfer绘制原始数据剖面平面图的构想,编制程序实现bln文件的创建,制作出规则测网和不规则测网的剖面平面图,取得了令人满意的效果。     

集对分析在西安市地下水污染动态评价的应用

选取总固体、总硬度、硝酸盐、氯化物、氟化物、六价铬等六种主要污染物,利用集对分析的方法,将超标率、污染指数和超标面积指数综合起来,对 1985-2003 年西安建成区地下水进行了动态评价.该方法既克服了依靠某年监测值对地下水质的静态空间评价,又可将超标率、污染指数和超标面积综合起来,完成地下水水质的动态评价.     

What Happened in the Trans-North China Orogen in the Period 2560-1850 Ma？

The Trans-North China Orogen （TNCO） was a Paleoproterozic continent-continent collisional belt along which the Eastern and Western Blocks amalgamated to form a coherent North China Craton （NCC）. Recent geological, structural, geochemical and isotopic data show that the orogen was a continental margin or Japan-type arc along the western margin of the Eastern Block, which was separated from the Western Block by an old ocean, with eastward-directed subduction of the oceanic lithosphere beneath the western margin of the Eastern Block. At 2550-2520 Ma, the deep subduction caused partial melting of the medium-lower crust, producing copious granitoid magma that was intruded into the upper levels of the crust to form granitoid plutons in the low- to medium-grade granite-greeustone terranes. At 2530-2520 Ma, subduction of the oceanic lithosphere caused partial melting of the mantle wedge, which led to underplating of mafic magma in the lower crust and widespread mafic and minor felsic volcanism in the arc, forming part of the greenstone assemblages. Extension driven by widespread mafic to felsic volcanism led to the development of back-arc and/or intra-arc basins in the orogen. At 2520-2475 Ma, the subduction caused further partial melting of the lower crust to form large amounts of tonalitic-trondhjemitic-granodioritic （TTG） magmatism. At this time following further extension of back-arc basins, episodic granitoid magmatism occurred, resulting in the emplacement of 2360 Ma, -2250 Ma 2110-21760 Ma and -2050 Ma granites in the orogen. Contemporary volcano-sedimentary rocks developed in the back-arc or intra-are basins. At 2150-1920 Ma, the orogen underwent several extensional events, possibly due to subduction of an oceanic ridge, leading to emplacement of mafic dykes that were subsequently metamorphosed to amphibolites and medium- to high-pressure mafic granulites. At 1880-1820 Ma, the ocean between the Eastern and Western Blocks was completely consumed by subduction, and the dosing of the ocean led to the continent-arc-continent collision, which caused large-scale thrusting and isoclinal folds and transported some of the rocks into the lower crustal levels or upper mantle to form granulites or eclogites. Peak metamorphism was followed by exhumation/uplift, resulting in widespread development of asymmetric folds and symplectic textures in the rocks.     

河北西北部熔积岩特征及其地质意义

熔积岩是火山碎屑岩的一种特殊类型，由熔浆和未固结的湿沉积物两种组分掺杂混合而成。熔积岩的形成主要受炽热熔浆与未固结的湿沉积物接触时引起的淬碎或蒸汽爆炸作用以及寄主沉积物流体化作用控制，通常分布于熔岩流底部或前缘，也可分布于超浅成侵人体周围。据熔浆碎屑物的结构特征，冀西北熔积岩可分为流状和块状两种类型。流状熔积岩多是熔浆与细粒沉积物混合的结果，块状熔积岩大多与粗粒沉积物相关。正确鉴别熔积岩对确定沉积作用与岩浆作用的时序、研究盆地发展演化历史具有重要意义。     

CAD/GIS集成方法在土地利用数据管理信息系统中的应用

随着信息技术交叉快速发展,多种技术相互借鉴并走向融合,是当前信息科学应用领域中的必然趋势。本文首先分析了CAD/GIS集成应用的必要性,接着阐述了CAD/GIS数据集成与功能集成的一般方法,以及在应用中存在的主要问题。然后,给出了一种数据解译器组成结构,可以有效地实现CAD/GIS数据的无缝集成。同时,提出了以组件技术实现CAD/GIS功能紧密集成的概念模式。最后,以土地利用数据管理信息系统开发为例,验证了CAD/GIS集成能明显提高信息系统的整体效能。     

基于Web GIS的上海数字农业集成系统

上海农业集成系统是基于JZ地理信息系统软件(精准农业信息公司开发的一套基于Web发布的地理信息系统发布引擎)开发的一套BS架构的农业系统。该平台采用了ASP.NET技术、SQL Server数据库管理技术以及地图发布引擎(JZ地图引擎)等技术,将传感器采集到的实时数据发布到网上,使各种不同目的的客户能够及时了解、分析和处理数据,并根据数据的实际情况及时应对农作物生长过程中的不良状态。本文对该平台的关键技术、数据管理、功能模块和安装步骤等方面作了详细的介绍。     

WGS-84与地方坐标系转换参数的优化选择

针对GPS动态RTK测量中WGS-84与本地坐标系转换参数的选择进行研究。首先根据稳健估计方法对控制点的精度进行评定,剔除含有粗差的控制点。然后利用概率统计理论对转换参数的优化选择进行分析,确定转换参数最优值。为便于实际应用,编写了转换参数优化选择软件,并将此软件的计算结果应用到实践中,取得较好结果,为证明该方法的可行性提供可靠依据。     

一种快速图像匹配方法的设计与实现

改进了遗传算法的编码,重新定义了交叉变异算子,结合运动估计中一种新的线性搜索方法--线性正方形搜索算法,实现了一种快速匹配算法,试验表明了算法的有效性和优越性.