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241.
WATERRESOURCESTRANSFORMATIONANDWATERQUALITYVARIATIONINTHEURUMQIRIVERBASINQuYaoguang(曲耀光);LuoHongzhen(骆鸿珍)(LanzhouInstituteofG... 相似文献
242.
WGS-84与北京54坐标的转换问题 总被引:53,自引:8,他引:45
GPS测量得到的是WGS-84中的地心空间直角坐标,而工程施工中通常使用地方独立坐标系,要求得到地方平面坐标。如何实现两者的转换,一直是工程施工中关心的热点问题。介绍了从GPS定位结果至平面坐标的两种转换模型。平面转换模型原理简单,数值稳定可靠,但只适用于小范围的GPS测量;空间转换模型可用于大范围GPS测量,按实际情况又分为7参数转换和3参数转换两种。鉴于54坐标点的大地高通常不能精确得知,对这两种转换方法得到的平面坐标的精度进行了比较,得出大地高精度主要表现为对高程的影响,对平面坐标影响较小的结论。此外,还讨论了7参数与3参数模型对转换结果的影响。 相似文献
243.
潮汐形变资料中地震前兆信息的识别与提取 总被引:30,自引:17,他引:13
将小波变换的多分辨率分析引入潮汐形变资料处理中,对近年来云南地区的3次强震前的潮汐形变观测资料进行了处理与分析,发现在地震前2~5个月,震中附近的形变台站都接收到一个频段相同的异常信号,且它们之间是相关的,相关系数达80%以上,由此可以确定信号是由同一个源发出来的。出现在多个台站的相同频段的异常信号很可能就是我们想要得到的地震前兆信息。 相似文献
244.
We present a new set of variables for the reduction of the planetary n-body problem, associated to the angular momentum integral, which can be of any use for perturbation theory. The construction of these variables is performed in two steps. A first reduction, called partial is based only on the fixed direction of the angular momentum. The reduction can then be completed using the norm of the angular momentum. In fact, the partial reduction presents many advantages. In particular, we keep some symmetries in the equations of motion (d'Alembert relations). Moreover, in the reduced secular system, we can construct a Birkhoff normal form at any order. Finally, the topology of this problem remains the same as for the non-reduced system, contrarily to Jacobi's reduction where a singularity is present for zero inclinations. For three bodies, these reductions can be done in a very simple way in Poincaré's rectangular variables. In the general n-body case, the reduction can be performed up to a fixed degree in eccentricities and inclinations, using computer algebra expansions. As an example, we provide the truncated expressions for the change of variable in the 4-body case, obtained using the computer algebra system TRIP. 相似文献
245.
In the present paper, inequalities stronger than Sundman's and the best possible zero velocity surfaces of the spatial 3-body problem first obtained by Saari (1987) are deduced using a modified version of the transformation developed by Zare (1976). The notion of inertia ellipsoid is used to show the equivalence of the present authors' result to that of Saari's. 相似文献
246.
L. MORTEN G. M. BARGOSSI J. M. MARTINEZ MARTINEZ E. PUGA A. DIAZ de FEDERICO 《Journal of Metamorphic Geology》1987,5(2):155-174
Abstract Several small bodies of metabasite (maximum dimensions of 1000 m x 500 m) are included in the metamorphic rocks of the Nevado-Filabride Complex in the Betic Cordilleras (Almeria Region). The body of 400 m x 100 m, located 200 m due west of the Lubrin village, contains troctolitic gabbro with well-preserved igneous textures and mineral compositions, wholly amphibolitized gabbro, garnet-bearing metagabbro eclogite. Along with the textural and mineral changes, sensible and regular geochemical variations can be observed, where the content of MgO decreases from 24% to 11%, while that of CaO and Na2O increases from 7% to 11% and from 2% to 3%, respectively. In addition, the content of some minor elements such as Sr, Y, Nb, Zr and Sc increases while that of Ni and Cr decreases from troctolitic gabbro to the eclogite. The amphibolitized gabbro shows values scattered around those of the troctolitic gabbro. These geochemical variations are ascribed to inherited differences in the pre-metamorphic protolith, i.e. a fractionated gabbro which varies from olivine-rich to clinopyroxene-rich gabbro. Nevertheless, some metasomatism affected the Lubrin body without changing the main chemical trends, as documented by the significantly different 87Sr/86Sr ratios of each rock-type. This points to a metasomatism which involved the introduction of crustal radiogenic strontium. The petrographical and mineral chemical features are interpreted to be the result of syn-metamorphic fluid circulation possibly combined with deformation by shearing. The igneous texture and mineral chemistry have been retained wherever both fluid circulation and shearing were ineffective. On the contrary, where both events were effective, the formation of eclogite occurred. Later, the entire body underwent a retrogressive amphi-bolitic stage under greenschist facies conditions, which was probably responsible for the formation of the amphibolitized gabbro portion and for the retrogression of the eclogite. 相似文献
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