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61.
无人机影像的重叠度通常较大(60%~80%),对纠正后的正射影像进行拼接处理时,往往会产生很大的数据冗余。同时,影像越靠近边缘处变形越大,影响拼接精度。提出了一种顾及有效区域的Voronoi图的拼接线自动选取方法,基于整体构建拼接线网络,并根据影像有效区域优化拼接线,保证拼接的精度和效率。实验表明,该方法切实可行。 相似文献
62.
Petr Zasche 《Astrophysics and Space Science》2005,296(1-4):127-130
Four eclipsing binaries, which show apparent changes of period, have been studied with respect to a possible presence of the
light–time effect. With a least squares method we calculated new light elements of these systems, the mass function of the
predicted third body, and its minimum mass. We discuss the probability of the presence of such bodies in terms of mass function,
changes in radial velocity and third light in solution of light curves. 相似文献
63.
何翔 《大地测量与地球动力学》1993,(1)
根据云南省楚雄、永胜台的倾斜矢量图在强震前正常年变化被破坏的事实,探讨了矢量图面积异常与地震的关系。认为矢量图所围面积的变化与地下水的作用固然有一定的关系,而起决定作用的是地震前应变积累的程度。倾斜矢量图面积的减小可以作为预报的一项参考指标。 相似文献
64.
云南昭通大型铅锌矿是滇东北矿集区乃至川滇黔铅锌成矿域铅锌矿床的典型代表。矿床具有明显的矿物组合分带性的特点,区别于典型的MVT型铅锌矿床。根据矿物组合特征构建、计算、绘制了该矿床的p H-logfo2、p Hloga相图,剖析了铅锌矿共生分异的形成机理。研究表明p H、氧逸度、组分浓度的协同作用造成了铅、锌的共生分异,对矿物组合分带起控制作用,且温度下降、氧逸度升高和p H升高有利于金属硫化物的沉淀,成功解释了昭通铅锌矿床独具特色的矿物分带地质特征。 相似文献
65.
66.
67.
详细介绍了Hipparcos测定的昴星团距离与以往地面测定结果比较所出现的差异、近年来对昴星团距离新的测定和对Hipparcos数据作的重新处理以及对造成不一致的原因所进行的探讨,最后对有关进展加以评述。 相似文献
68.
Aaron J. Grocholski Ata Sarajedini 《Monthly notices of the Royal Astronomical Society》2003,345(3):1015-1029
We present combined optical/near-infrared photometry ( BVIK ) for six open clusters – M35, M37, NGC 1817, NGC 2477, NGC 2420 and M67. The open clusters span an age range from 150 Myr to 4 Gyr and have metal abundances from [Fe/H]=−0.27 to +0.09 dex. We have utilized these data to test the robustness of theoretical main sequences constructed by several groups as denoted by the following designations – Padova, Baraffe, Y2 , Geneva and Siess. The comparisons of the models with the observations have been performed in the [ MV , ( B − V )0 ], [ MV , ( V − I )0 ] and [ MV , ( V − K )0 ] colour–magnitude diagrams as well as the distance-independent [( V − K )0 , ( B − V )0 ] and [( V − K )0 , ( V − I )0 ] two-colour diagrams. We conclude that none of the theoretical models reproduces the observational data in a consistent manner over the magnitude and colour range of the unevolved main sequence. In particular, there are significant zero-point and shape differences between the models and the observations. We speculate that the crux of the problem lies in the precise mismatch between theoretical and observational colour–temperature relations. These results underscore the importance of pursuing the study of stellar structure and stellar modelling with even greater intensity. 相似文献
69.
Properties of iron at the Earth's core conditions 总被引:2,自引:0,他引:2
Orson L. Anderson 《Geophysical Journal International》1986,84(3):561-579
Summary. The phase diagram of iron up to 330 GPa is solved using the experimental data of static high pressure (up to 11 GPa) and the experimental data of shock wave data (up to 250 GPa). A solution for the highest triple point is found ( P = 280 GPa and T = 5760 K) by imposing the thermodynamic constraints of triple points. This pressure of the triple point is less than the pressure of the inner core–outer core boundary of the Earth. These results indicate that the density of iron at the inner core–outer core boundary pressure is close to 13 g cm−3 , which lies close to the seismic solutions of the Earth at that pressure. It is thus concluded that the Earth's inner core is very likely to be virtually pure iron in its hexagonal close packed (hcp) phase.
It is shown that four properties of the Earth's inner core determined from seismology are close in value to the corresponding properties of hcp iron at inner core conditions: density, bulk modulus, longitudinal velocity, and Poisson's ratio. The density–pressure profile of hcp iron at inner core conditions matches the density–pressure profile of the inner core as determined by seismic methods, within the spread of values given by recent seismic models.
This indicates that the Earth is slowly cooling, the Earth's inner core is growing by crystallization, and the impurities of the core are concentrated in the outer core. The calculated temperature at the Earth's centre is 6450 K. 相似文献
It is shown that four properties of the Earth's inner core determined from seismology are close in value to the corresponding properties of hcp iron at inner core conditions: density, bulk modulus, longitudinal velocity, and Poisson's ratio. The density–pressure profile of hcp iron at inner core conditions matches the density–pressure profile of the inner core as determined by seismic methods, within the spread of values given by recent seismic models.
This indicates that the Earth is slowly cooling, the Earth's inner core is growing by crystallization, and the impurities of the core are concentrated in the outer core. The calculated temperature at the Earth's centre is 6450 K. 相似文献
70.
中国大陆7级强震前地下流体前兆时空特征 总被引:5,自引:0,他引:5
对中国大陆1969年以来11次7级强震前地下流体前兆观测资料分阶段进行统计分析,并选用雷达图描述了中国大陆7级强震前地下流体前兆异常的时空特征,认为其特征主要表现在:异常出现时间上的阶段性与不均匀性,中长期趋势性异常分散,短临异常相对集中,且各占总异常比例的50%左右;震前异常集中在一定的范围内,并沿活动断裂呈现出一定的集中性;中长期趋势异常较早出现在震源区附近,并呈现出由震源区向外围扩散-收缩-扩散-收缩的过程,特别是进入短临阶段后,异常向震源区收缩的趋势更为明显;在震源区(或在距震源较近的范围内)异常所占的比例大,远离震源区所占比例小,且有由震源区向外围逐渐减小的趋势。 相似文献