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排序方式: 共有3484条查询结果,搜索用时 93 毫秒
201.
Kuniaki Abe 《Pure and Applied Geophysics》2007,164(2-3):453-463
We identified a phase representing the source length of tsunami's in the tide gauge records around Japan. This phase was observed
at tide stations, located in the direction of the long axis of the sources, for four large tsunamis: 1964 Niigata, 1968 Tokachi-oki,
1983 Nihonkaichubu, and 1993 Hokkaido-nanseioki. The phase consists of two continuous crests starting as the initial arrival
and has a time length of 15–47 minutes. This is the time required to propagate across the source area along the long axis.
Strong evidence that the phase is generated at the source is the good correlation between waveform observed at one side and
time-inversed waveform at another side. The correlation results from the instantaneous generation of the source. The source
lengths of 74–254 km were obtained under an assumption of sea depths at the sources and verified to coincide with ones within
a relative error of 15% that were previously obtained by other methods. 相似文献
202.
一种附约束的单频单历元GPS双差相位解算方法 总被引:8,自引:1,他引:8
在各类变形观测中,存在着2次观测的变形值不大及各种变形方向和大小可以比较精确预测等特点,可以把这些特征作为约束条件,对GPS单历元相位观测方程进行求解。基于以上几点,提出了一种含约束条件的单频单历元GPS相位求解算法和简单实用的模糊度搜索方法,本方法据观测值直接估计模糊度参数,并根据求出的模糊度估值进行搜索,还分析了最优解的获得和检验方法,最后用2个实例说明了该法的有效性和实用性。 相似文献
203.
相位激电法(偶极-偶极)单频电磁耦合校正方法 总被引:2,自引:2,他引:2
主要介绍一种相位激电法(偶极—偶极,以下简称偶极)电磁耦合校正方法,其原理是将视电阻率近似视为均匀大地电阻率,利用均匀大地条件下偶极装置电磁感应响应的正演计算方法,算出电磁感应响应,再将其从观测的总响应中去除,从而达到电磁耦合校正的目的。 相似文献
204.
闽台地震速报技术研究 总被引:1,自引:0,他引:1
本文通过系统地分析台网正式运行以来记录到主要的网内、网缘、网外地震的各种震相特征和定位参数 ,总结研究各区的震相特征、台站记录状况和震级的误差 ,力争提高台网地震速报的速度和精度。 相似文献
205.
本文通过分析福州、小陶地震的波形记录及各种定位参数 ,总结了该地区的震相特征和各台的震级情况 ,结合地震速报的规程 ,提出了对这两个地区地震速报的建议。 相似文献
206.
对黄磷电炉烟尘中各种形态的磷化合物进行了化学物相分析,得出元素磷、水溶性低价磷化合物、水溶性高价磷化合物、酸溶性高价磷化合物、酸溶性低价磷化合物、酸不溶性磷化合物在黄磷电炉烟尘中的含量,并对黄磷电炉烟尘的综合利用提出了建议。 相似文献
207.
Developing a bivariate spatial association measure: An integration of Pearson's r and Moran's I 总被引:1,自引:0,他引:1
Sang-Il Lee 《Journal of Geographical Systems》2001,3(4):369-385
This research is concerned with developing a bivariate spatial association measure or spatial correlation coefficient, which
is intended to capture spatial association among observations in terms of their point-to-point relationships across two spatial
patterns. The need for parameterization of the bivariate spatial dependence is precipitated by the realization that aspatial bivariate association measures, such as Pearson's correlation coefficient,
do not recognize spatial distributional aspects of data sets. This study devises an L statistic by integrating Pearson's r as an aspatial bivariate association measure and Moran's I as a univariate spatial association measure. The concept of a spatial smoothing scalar (SSS) plays a pivotal role in this task.
Received: 07 November 2000 / Accepted: 02 August 2001 相似文献
208.
209.
本文通过对塔里木盆地轮南地区及附近的钻井(出油井和未出油井)中揭示的裂缝,裂缝与成岩序列的穿插关系,连通砂体及断层和不整合面附近的矿物及矿物中流体包裹体研究,对塔里木盆地轮南地区油气运移路径和期次进行了探讨。通过研究指出了塔里木盆地轮南地区主要经历了3期大规模的油气运聚,地层之间的不整合面为油气横向运移的主要通道。高角度的裂隙及微裂缝为纵向运移主要通道。第一期油气运聚主要发生于海西期,第二期油气运聚主要发生在14-17Ma;第3期油气运聚主要发生在最近的5Ma以来。第一期油气运聚主要为自塔北隆起的西南,南向北,以横向运移为主;第二,第三期运聚主要自西南,南向北,自东向西运移,但主要以垂向运移为主。 相似文献
210.
Jeroen van Hunen Arie P van den Berg Nico J Vlaar 《Earth and Planetary Science Letters》2001,190(3-4):125-135
Very low to zero shallow dip angles are observed at several moderately young subduction zones with an active trenchward moving overriding plate. We have investigated the effects of latent heat for this situation, where mantle material is pushed through the major mantle phase transitions during shallow low-angle subduction below the overriding plate. The significance of the buoyancy forces, arising from the latent heat effects, on the dynamics of the shallowly subducting slab is examined by numerical modeling. When a 32-Ma-old slab is overridden with 2.5 cm/yr by a continent, flat subduction occurs with a 4–5 cm/yr convergence rate. When latent heat is included in the model, forced downwellings cause a thermal anomaly and consequently thermal and phase buoyancy forces. Under these circumstances, the flat slab segment subducts horizontally about 350 km further and for about 11 Ma longer than in the case without latent heat, before it breaks through the 400-km phase transition. The style of subduction strongly depends on the mantle rheology: increasing the mantle viscosity by one order of magnitude can change the style of subduction from steep to shallow. Similarly, an overriding velocity of less than 1 cm/yr leads to steep subduction, which gradually changes to flat subduction when increasing the overriding velocity. However, these model parameters do not change the aforementioned effect of the latent heat, provided that low-angle subduction occurs. In all models latent heat resulted in a substantial increase of the flat slab length by 300–400 km. Varying the olivine–spinel transition Clapeyron slope γ from 1 to 6 MPa/K reveals a roughly linear relation between γ and the horizontal length of the slab. Based on these results, we conclude that buoyancy forces due to latent heat of phase transitions play an important role in low-angle subduction below an overriding plate. 相似文献