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991.
992.
2017年8月8日九寨沟发生7.0级地震,此次地震发生在塔藏断裂、岷江断裂和虎牙断裂附近,震源机制为走滑型。重力场静态异常和动态异常变化可为研究深地壳结构性质提供重要的物理场信息。本文利用WGM计算的布格重力异常数据及实测流动重力数据进行小波多尺度分解,分离得到不同深度场源特征的地壳介质横向不均匀性。结果表明,WGM布格重力异常数据和实测重力数据的小波多尺度结果较为一致,通过对比分析发现,九寨沟地震发生在区域重力场的四象限分布中心位置,不同时空尺度的重力场变化对于深入认识潜在地震危险性趋势具有一定的科学意义。 相似文献
993.
AbstractThis article applies open source data of public facilities through data mining, not only to evaluate the public facilities from an objective dimension, but also to reflect the sensory opinions of the group factually, eventually realizing the evaluation measurement of urban public facilities. The research takes Shenzhen city as an empirical case and chooses typical public facilities to mine data, resolve address and weight to explore the application of public facilities evaluation under dimension reduction of open source data. The empirical study consists of three parts. First, as the objective evaluation, we estimate the density distribution and per capita of public facility through data mining and address resolution. Second, as the subjective evaluation, we carry on the location analysis to high-score public facility through attention and satisfaction data of Internet evaluation. Finally, as mentioned above, we calculate the weight of objective and subjective evaluation of public facility, eventually formatting the comprehensive evaluation of public facilities. 相似文献
994.
在航空电磁探测方法应用中,地下探测环境复杂,地下介质物性参数存在各向异性特征。如果采用常规各向同性介质模型,在资料解释过程中会产生严重的偏差。本文基于矢量有限元法开展三维任意各向异性频率域航空电磁响应模拟计算研究。首先,将总场分解成一次场和二次场,对空气介质的均匀全空间进行一次场解析计算,同时利用矢量有限元法对二次电场的双旋度方程进行求解。为提高求解速度,采用共享内存直接求解器PARDISO对大规模稀疏矩阵并行计算,大大提高了三维模型的计算速度。之后开展了4种典型目标模型的三维各向异性介质模拟:围岩各向同性-目标体各向异性(绕z轴旋转)模型;围岩各向同性-目标体各向异性(绕x轴旋转)模型;围岩各向异性-目标体各向异性(绕z轴旋转)模型;围岩各向异性-目标体各向异性(绕x轴旋转)模型。对比分析了不同模型在不同旋转角度情况下,磁场实虚分量的变化特征,进而总结了各向异性参数对航空电磁响应的影响规律和识别方法。 相似文献
995.
???÷?????????????ü??????????????????????????GEMT3??JGM3??EGM96??TEG4??EIGEN2??EIGEN??GL04C??????????????????????????????????????????????????????????????????????????????????????????????????????????????????????н???????????CHAMP ??GRACE?????????????????????????????????????????????????????????????????cm????????22.47 cm????????????к??????? 相似文献
996.
GPS载波相位三差观测方程的改化 总被引:3,自引:0,他引:3
本文根据相关测量平差原理推导出改化GPS载波相位三差观测方程的算法,使改化后的协因数呈分块对角体。这种改化算法不但顾及观测值的相关性,而且节省大量的存储单元。使采用严密平差法平差三差观测值成为一种最简单的数据处理方法之一。 相似文献
997.
998.
On the basis of observations and results from the combination of a statistical formation model and a trajectory model, the inter-decadal shift of prevailing TC tracks in the western North Pacific (WNP) are examined. The contributions of the changes in large-scale steering flows and tropical cyclone (TC) formation locations to the observed inter-decadal shift are investigated and their relative importance is determined. This study focuses on two periods, 1965–1986 (ID1) and 1987–2010 (ID2), which are determined based on the abrupt change of the annual category 4 and 5 TC frequency derived from the Bayesian change-point detection analysis. It is found that the models can well simulate the primary features of prevailing TC tracks on the inter-decadal timescale. From ID1 to ID2, a significant decrease in the frequency of TC occurrences is observed over the central South China Sea and well simulated by the models. Areas with a remarkable increase in the TC frequency, which extends from the Philippine Sea to the eastern coast of China and in the west of the WNP basin, are also reasonably simulated. Above changes in the prevailing TC tracks are attributed to (1) intensified cyclonic circulation centered over the western part of China and (2) more westward-southward expansion and intensification of the subtropical high over the WNP. Further analysis reveals that the inter-decadal shift in prevailing TC tracks is mainly resulted from the combined effects of changes in large-scale steering flows and TC formation locations. Although both contribute to the inter-decadal shift in the prevailing TC tracks, changes in large-scale steering flows play a more important role compared to changes in TC formation locations. 相似文献
999.
In this article,we use the CAP method to invert the focal mechanism of Xinyuan-Hejing M S6. 6 earthquake on June 30,2012. Our result shows that the best double couple solution of the M S6. 6 event is 299°,68° and 164° for strike,dip and rake angles respectively. The other nodal plane is 35°,75° and 23°. The azimuth and dip angle of the P-axis are 166°and 5°,those of the T-axis are 258° and 26°. The moment magnitude is 6. 3. The estimated focal depth is about 21 km. The predominant rupture direction of this seismic sequence is NWW. The dip angles are between 60° and 90°. The rake angles are in the majority of ± 180°± 30°. The predominant strike of the azimuthal angle of the P-axis is near NS and T-axis is near EW. Preliminary analysis indicates that nodal plane I is the seismogenic fault,which is a NWW-trending,nearly upright left-lateral strike-slip fault.The displacement property,the principal compressive stress of this M S6. 6 earthquake and the P-axis preponderant orientation of this seismic sequence agree with the characteristics of the tectonic stress field of the focal area and its surroundings. 相似文献
1000.
本文对周口店新发现距今11~1.9万年的东岭子洞穴堆积物进行了成因研究,认为该套堆积物并非全属岩溶堆积物,其中也有风成黄土沉积。应用古地磁、热发光及铀系法等年代学方法测定,认为这套堆积为距今11~1.9万年间沉积,弥补了周口店地区近5万年的晚更新世洞穴地层空缺,是一个含有丰富地质事件的晚更新世洞穴地层剖面。 相似文献