查询词典 receiver

Limited to the environment , the traditional used hydrologic telemetric equipment are data transmitter and ultra-short wave transmitter-receiver.

由于水文自然环境的限制，传统测报主要使用数传仪、超短波电台等测报设备。

Up to now, all of the methods of isolating the receiver function from teleseismic P waves are based on the data recorded at a single station.

迄今为止，广泛应用的分离接收函数方法主要基于单个台站的观测数据，并依赖等效震源假定的有效性。

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。

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。

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。

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。

Based on the large amount of teleseismic waveform data recently collected in North China, we are to construct high-resolution seismic images for the lithosphere and upper mantle structure of the region using the newly developed receiver function wave equation poststack migration technique.

利用华北地区丰富的远震波形资料，采用最近发展的远震接收函数波动方程叠后偏移成像方法，研究该地区岩石圈和上地幔的高分辨率结构图像。

In this paper, those teleseismic records with clear P waveforms are chosen to carry out receiver function analysis and modeling. A simple crustal structure model beneath the station is obtained, in which the Moho depth is 28 km. On the top of the upper crust is a 2 kmthick low velocity layer with a shear wave velocity of only 23 km/s. The shear wave velocity increases gradually with depth to 38 km/s in the lower crust.

本文对具有清晰P波波形的远震记录进行了接收函数处理和计算模拟，得到台站下简单的地壳结构模型，其莫霍面深度为28 km，上地壳顶部有一层2 km厚的低速层，横波速度只有23 km/s，向下逐渐过渡到横波速度为38 km/s的下地壳。

On the other hand, the more important thing is because the urban housing is a kind of heterogeneity products.

另一方面，更重要的是由于城市住房是一种异质性产品。

Climate histogram is the fall that collects place measure calm value, cent serves as cross axle for a few equal interval, the area that the frequency that the value appears according to place is accumulated and becomes will be determined inside each interval, discharge the graph that rise with post, also be called histogram.

气候直方图是将所收集的降水量测定值，分为几个相等的区间作为横轴，并将各区间内所测定值依所出现的次数累积而成的面积，用柱子排起来的图形，也叫做柱状图。