全数字摄影测量室内判调方法的应用     

夏荣  弓美荣 《测绘技术装备》2007,9(1):42-43

本文阐述了航测法成图制作1:1万地形数据工作过程中,采用全数字摄影测量工作站对地物进行室内判调“先内后外”的作业方法,并通过对获取的成果与常规方法的对比,证明此法在实际生产中具应用价值。  相似文献   

90年代加拿大移民地区结构新特点     

杜德斌 《世界地理研究》1998,(2)

90年代是战后以来加拿大移民的高峰时期,本文总结了这一时期加拿大移民来源地和居住分布的新特点。其突出表现是：亚洲已成为加拿大最大的移民来源地,其中来自香港、中国大陆和台湾的华人成为最大的移民群体;移民选择大城市,尤其是多伦多、温哥华和蒙特利尔三大都市区作为定居地的倾向进一步加强。  相似文献   

博洛科努断裂西北段古地震形变带初步研究   总被引：4，自引：0，他引：4  

沈军  杨小平 《内陆地震》1998,12(3):248-255

介绍了博洛科努断裂西北段阿拉山口至精河县城以南的古地震形变带的几何特征、形变方式和变形幅度,并讨论了最后一次地震事件的震级。认为该形变带为右旋走滑性质,最后一次地震事件的水平位移可能为２．５ ｍ ,垂直位移为０．９～１．８ ｍ ,震级估计为７．５～７．８ 级  相似文献   

云南三江并流地区气候变化及其对生态环境的影响   总被引：4，自引：1，他引：4  

郭菊馨  王自英  白波  鲁亚斌 《云南地理环境研究》2006,18(2):48-52

利用EOF等方法通过计算1971-2000年30年来云南三江并流地区6个气象台站气温、降水、蒸发资料，分析了云南三江并流地区近30年来气候变化的异常特征及其对生态环境的影响，结果表明：云南三江并流地区气候变化表现为气温升高、降水略有减少和蒸发增大的干旱化气候变化趋势，同时，在气候干旱化和人为活动的影响下出现草场退化、冰川萎缩、雪线上升、土壤沙化和水土流失等生态环境荒漠化问题。  相似文献   

随深度指数变化的视电阻率解     

梁子斌  钱家栋 《高原地震》1998,(2)

从横向均匀介质满足的基本方程出发,得到视电阻率核函数的一阶非线性微分方程,通过方程求解,并利用滤波系数法容易得到电阻率随深度任意变化的视电阻率问题。当各层介质电性结构随深度呈指数变化时,还可得到各层之间核函数的递推关系,这对实际介质的正反演问题都有重要意义和应用价值。  相似文献   

地震综合前兆场建场方法初探          下载免费PDF全文

夏玉胜  梁子斌  蔡红卫  张慧  杨丽萍  张敏 《地震工程学报》1998,20(1):42-46

初步建立了一种能反映地震前兆时空演化全貌的无量纲、归一化可迭加的信息场———综合前兆场．通过对研究区（东经１１３°～１２５°,北纬３２°～４４°）前兆场时空演化过程的分析发现,地震前前兆场由正常的低值离散逐渐发展为围绕震中呈高值封闭状态,震后恢复正常．该方法的独特之处在于,避开了某些单项异常对应某具体源的分析,而是只考虑异常．根据前兆场的变化可以确定震源的大致位置  相似文献   

西藏东部大气降水氧同位素组成特征   总被引：24，自引：0，他引：24  

于津生张鸿斌  虞福基刘德平 《地球化学》1980,(2):113-121

The Xizang Plateau, with a common altitude of more than 4000 m sbove sea level,has long been celebrated as “The Roof of the World”. In order to study oxygen isotopic composition of meteoric water in the Xizang Plateau Region and its relationship with the attitude, we made an investigation tour to the Xizang Plateau, starting from Guizhow, during 1979 from July to October, and 79 meteoric Water samples were collected, including brook, well, lake, snow, firn, spring and running waters, at different altitudes. Oxygen isotope analyses indicate that the isotopie composition of meteoric water in the areas more than 4000g and in the western parts of SichuanGaizhow shows remarkable altitude effect. There is a negative correlation between δ^28O and altitude, which is reflected by --δ^18O = 0.0026H 7.75. The average δ^18O value for metcoric water in the areas: more than 4000m above sea level turns out to be --18.15‰ is evident that δ^18O value for lake water on the plateau is related to its water supply. δ^18O value for lake water, in which the evaporation is greater than supply,is approximately three or four times higher than that of supplied water, averaging -5.74‰. Oxygen isotopic compasition of geothermal water can be compared with that of local meteoric water, but shows certain δ^18O-shift, suggesting that the main water-supply source seems to be meteoric water in the same area.  相似文献   

SESAM锁模激光器在卫星激光测距领域应用研究     

卫志斌  瞿锋  项清革  李谦 《测绘科学》2009,34(6)

本文在分析SESAM(Semiconductor Saturable Absorber Mirrors)锁模激光器原理及技术特点、描述其工作流程的基础上,展示了SESAM锁模激光器用于卫星激光测距的实测结果,通过对卫星激光测距数据数量及质量分析,得出了SESAM锁模激光器以窄脉冲宽度、高能量密度、输出稳定等优势首次在国内应用于卫星激光测距系统后,使系统整体性能得到明显提升的结论。  相似文献   

孟州:"农民公寓"解决农民用地难     

张泽斌  郝永利 《资源导刊(河南)》2009,(12)

"我们家在仅有的一分宅基地上,两座砖土混合结构的老房屋里生活了几代人,想再申请一处大一点的宅基地,可村里实在没有一点空余地方了,所以家里四口人只能凑合着居住.不过现在可好了,村里考虑到我家的实际情况,优先给我们提供了二楼,面积115平方米,9万多元就拿到手的平价房.  相似文献   

华南某花岗岩型铀矿床成矿机理的铀铅同位素体系研究     

李耀菘  李喜斌 《地球化学》1985,(1):20-26

The uranium deposit studied in this paper occurs in a Precambrian (Xuefengian)granite batholith. The emplacement age of the granite is 760 m.y. The average content of uranium in the granite is 7 ppm, but the yield of leachsd U is higher With an average of about 33.8%. The granitic rocks, contain; Some uraninite. Uranium mineralization mainly takes the form of siliceous veins With an age of 47 m.y. K-feldspar. present in the granite and pyrite associated with pitchblende were massspectrometrically analyzed for Pb isotopic compositious, characterized by anomalous lead. A reasonably linear array can be seen on the ^207Pb/^206Pb--^205Pb/^204Pb plot, implying a genetic connection between the rock and the ore, and a derivation of rock-forming materials from. a uranium-rich source. According to the continuous-growth model for anomalous lead, evolution, two isochrons give the. ages-of about 764 m.y. and 708 m.y.for ore-forming materials, close to the emplacement age of .the granite batholith. This indicates that the ore-forming materials came from the granite batholith. Eight granite samples collected from the mining .area were analyzed, but no uranium-lead ages could be worked out because of the pregressive destruction of the closed U-Pb isotopic system since granite emplacement, which resulted in the loss of uranium(78%). It can be imagined that in the period of continental weathering the surface water would infiltrate downwards, leaching out large amounts of uranium from the granitic rocks to form infiltration solution. The solution was heated at great depth and then found its way upwards, on which it dissolved constantly U from the rocks to form the uranium deposit.  相似文献