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teleseismic相关的网络例句

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与 teleseismic 相关的网络例句 [注:此内容来源于网络,仅供参考]

Using the teleseismic waveforms recorded by the passive seismic experiment, receiver function method was used to investigate the S wave velocity structure.

利用记录到的远震体波波形资料和接收函数方法获得了剖面下0~100km深度的地壳和上地幔S波速度结构。

In chapter 1,we used broadband teleseismic data of ChingFeng station to calculate the Receiver Functions,then obtained a velocity model with H-K stacking method in combination with Crust2.0 and other previous work.

在本文的第一、二章中我们回顾了震源参数反演方法的发展,并详细介绍了几种主要的反演方法。

At the first step,experiments conducted on synthetic data are used to assess the ability to recover rupture slip details and teleseismic body waves.

使用的是一种基于小波变换的模拟退火非线性反演方法,我们将主断层划分成若干个小的子断层,在反演时同时确定每个子断层上的滑移量、滑动角、上升时间以及平均破裂速度。

We note that imaging dipping or curving interface is controlled by teleseismic azimuth, and receiver functions from different direction should be jointed to better resolve those complicated structures.

一个很重要的现象是,倾斜或弯曲界面的成像明显受控于远震的入射方向,其成像精度的提高有赖于不同方向接收函数的联合成像。

Anautomatic phase picker for local and teleseismic event.

基于小波包变换的信号突变检测、滤波和瞬态谱研究。

Keywords: Xisha Block; Earthquake observation; Teleseismic event; Receiver function; Crustal structure

中文关键词:西沙地块,地震观测、远震事件、接收函数、地壳结构

The space between stations is about 3-20 km.The crust and upper mantle structure down to 100 km deep along our profile is obtained from our teleseismic waveform data in terms of the receiver function method.

利用记录的远震P波波形数据和接收函数方法,获得了沿剖面100km深度范围内地壳上地幔S波速度结构以及地壳上地幔一级间断面的形态。

Tests of record type,source duration,attenuation factors of P and S body waves are made for sensitivity study of moment magnitude.After weighting regional data and teleseismic data properly according to their amplitudes,they can be used together in a Cut and Past inversion process.

本文第四章中我们对新近发展的CAPloc方法进行了一系列的测试,即在稀疏台网的条件下得到地震的震源机制解,并将其与利用整个TriNet数据反演得到的机制解进行对比,分析了单台和双台反演的稳定行和可靠性。

In this study we systemically investigate the effects of laterally inhomogeneous crustal structure with planar dipping interfaces on the teleseismic receiver function.

系统研究了台站下方存在倾斜界面时,远震体波接收函数的波场特征及多方位接收函数对台站下方介质横向非均匀特征的反映能力。

Clearly identifiable depth phases recorded by the teleseismic stations obviously provided a better constraint on the resulting source depth.

随后结合远震信号中的直达P、pP、sP波形得到了分辨率较高的地震震源深度。

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Finally, according to market conditions and market products this article paper analyzes the trends in the development of camera technology, and designs a color night vision camera.

最后根据市场情况和市面上产品的情况分析了摄像机技术的发展趋势,并设计了一款彩色夜视摄像机。

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只有半人深的荒草和龇牙咧嘴的神像。

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这一引人注目的地域范围,比喜马拉雅山更加陡峭,是处于西藏东部边缘的朝上翻的边框地带。响应启始于约5500万年前的、缓慢的但却不可阻挡的印度与亚洲地壳板块碰撞,高原已上升至五千米,这种碰撞持续至今,毫无衰退。