基于3G技术的空间物流仿真实验原型系统的设计与实现     

霍亮  任利娟  高艾凤 《测绘通报》2008,(10)

物流作为物体在时间和空间的位移,对地理空间具有较强的依赖件,3G技术与现代物流管理技术的有效集成已成为现在物流管理的重要趋势之一.基于3G技术,采用Swarm软件包,对空间物流信息平台的部分功能进行原型系统仿真实验.实验结果证明,该方法可以较好地对空间物流信息系统进行仿真模拟,对于信息平台的分析、设计及实施等具有一定的指导意义.  相似文献   

一种阵列式海洋磁力测量系统   总被引：1，自引：0，他引：1  

宗发保  邓瑞辉  任来平  顾建松  邹鹏毅  余恺 《海洋测绘》2015,35(1):45-47

基于多台海洋磁力仪、测深仪和GPS,研制了数据合成器、水下拖体、电源适配器、数据收录兼导航软件,最终构建了一种阵列式海洋磁力测量系统。该阵列式海洋磁力测量系统具备3个磁力仪通道,动态噪声≤0.3n T p-p,采样率为10Hz,水下部分总重量≤95kg,配迫降翼后入水深度可达22m。该阵列式磁力测量系统曾被应用于董家口港区某锚地的未爆炸物探测,最终确定了多个疑似物位置。  相似文献   

Geochronology, Geochemistry and Tectonic Setting of the Bairiqiete Granodiorite Intrusion (Rock Mass) from the Buqingshan Tectonic Mélange Belt in the Southern Margin of East Kunlun   总被引：1，自引：0，他引：1  

LI Zuochen  PEI Xianzhi  LI Ruibao  PEI Lei  LIU Chengjun  CHEN Youxin  LIU Zhanqing  CHEN Guochao  XU Tong  YANG Jie  WEI Bo 《《地质学报》英文版》2014,88(2):584-597

This study focuses on the zircon U–Pb geochronology and geochemistry of the Bairiqiete granodiorite intrusion(rock mass) from the Buqingshan tectonic mélange belt in the southern margin of East Kunlun. The results show that the zircons are characterized by internal oscillatory zoning and high Th/U(0.14–0.80), indicative of an igneous origin. LA–ICP–MS U–Pb dating of zircons from the Bairiqiete granodiorite yielded an age of 439.0 ± 1.9 Ma(MSWD = 0.34), implying that the Bairiqiete granodiorite formed in the early Silurian. Geochemical analyses show that the rocks are medium-K calc-alkaline, relatively high in Al2O3(14.57–18.34 wt%) and metaluminous to weakly peraluminous. Rare-earth elements have low concentrations(45.49–168.31 ppm) and incline rightward with weak negative to weak positive Eu anomalies(δEu = 0.64–1.34). Trace-element geochemistry is characterized by negative anomalies of Nb, Ta, Zr, Hf and Ti and positive anomalies of Rb, Th and Ba. Moreover, the rocks have similar geochemical features with adakites. The Bairiqiete granodiorite appears to have a continental crust source and formed in a subduction-related island-arc setting. The Bairiqiete granodiorite was formed due to partial melting of the lower crust and suggests subduction in the Buqingshan area of the Proto-Tethys Ocean.  相似文献   

The Petrology, Geochemistry, and Petrogenesis of E-MORB-type Mafic Rocks from the Guomangco Ophiolitic Mélange, Tibet     

XU Mengjing  LI Cai  WU Yanwang  XIE Chaoming 《《地质学报》英文版》2014,88(5):1437-1453

The Guomangco ophiolitic melange is situated in the middle part of the Shiquanhe- Yongzhu-Jiali ophiolitic melange belt （SYJMB） and possesses all the subunits of a typical Penrose- type ophiolite pseudostratigraphy. The study of the Guomangco ophiolitic melange is very important for investigating the tectonic evolution of the SYJMB. The mafic rocks of this ophiolitic melange mainly include diabases, sillite dikes, and basalts. Geochemical analysis shows that these dikes mostly have E-MORB major and trace element signatures; this is the first time that this has been observed in the SYJMB. The basalts have N-MORB and IAB affinities, and the mineral chemistry of harzburgites shows a composition similar to that of SSZ peridotites, indicating that the Guomangco ophiolitic melange probably originated in a back-arc basin. The Guomangco back-arc basin opened in the Middle Jurassic, which was caused by southward subduction of the Neo-Tethys Ocean in central Tibet. The main spreading of this back-arc basin occurred during the Late Jurassic, and the basalts were formed during this time. With the development of the back-arc basin, the subducted slab gradually retreated, and new mantle convection occurred in the mantle wedge. The recycling may have caused the metasomatized mantle to undergo a high degree of partial melting and to generate E- MORBs in the Early Cretaceous. E-MORB-type dikes probably crystallized from melts produced by about 20%-30% partial melting of a spinel mantle source, which was metasomatized by melts from low-degree partial melting of the subducted slab.  相似文献   

甘肃大型变形构造及蛇绿构造混杂岩带特征   总被引：1，自引：0，他引：1       下载免费PDF全文

梁明宏  张新虎  刘建宏  丁仨平  贾志磊 《甘肃地质》2014,23(4):1-8

大型变形构造带是地球表层重要的构造现象,它们记载了地壳的构造变形（走滑错移、逆冲叠覆和伸展滑移）过程及其动力学机制。本文根据大型变形构造定义及其分类原则,将甘肃省大型变形构造划分为3大类10种类型,初步厘定出大型变形构造带23个,简要叙述了主要大型变形构造规模、产状、构造层次、物质组成、变形期次等基本特征,探讨了大型变形构造与蛇绿构造混杂岩带的关系,从全省北山造山带、祁连造山带、西秦岭造山带和鄂尔多斯盆地“三带一盆”的构造格局出发,探讨大型变形构造形成、演化历史。  相似文献   

PM_(2.5)降尘诱导A549细胞G2/M期阻滞的机制研究     

杨洁  霍婷婷  王玉琳  董发勤  曾娅莉  邓建军 《岩石矿物学杂志》2017,36(6):894-902

PM_(2.5)降尘作用于A549细胞后,MTT法检测细胞存活率,扫描电镜观察细胞形态,流式细胞术检测细胞周期改变,RT-PCR检测周期阻滞相关基因p53、p21、CDK1、c-myc和lncRNA H19的表达水平,Western-blot检测周期蛋白cyclin B1表达。通过转染H19 siRNA干扰H19的表达,RT-PCR检测其对p53、c-myc及CDK1表达的影响,以探讨PM2.5降尘诱导A549细胞周期阻滞的作用机制。结果显示,PM2.5降尘暴露可降低A549细胞存活率,随作用浓度及时间增加呈递减趋势,并可观察到细胞形态破坏,细胞膜表面吸附聚集大量粉尘颗粒。PM2.5作用于细胞24 h后,A549细胞增殖阻滞在G2/M期,周期阻滞相关基因p53、p21及H19表达增加,CDK1及cyclin B1表达降低。此外,转染H19 siRNA后成功干扰H19的表达,并调控CDK1表达进一步降低。综合以上结果,PM2.5降尘处理A549细胞后可通过激活p53及p21活性,抑制CDK1和cyclin B1表达水平,诱导G2/M期阻滞从而抑制细胞增殖。短期暴露于PM2.5后,lncRNA H19在染毒细胞中可能发挥特异性癌基因的作用,通过与p53及c-myc结合参与调控细胞周期,干扰H19低表达使细胞G2/M期阻滞更加明显。  相似文献