1) Aftershock depths
余震深度
2) aftershock magnitude
余震强度
1.
1 Kunlun Mountain earthquake on November 14, 2001, is examined in this paper on the basis of a statistical research on relationship between the Corioli force effect and the maximum aftershock magnitude of 20 M ≥7.
5级以上特大地震余震强度与科里奥利力效应关系的统计研究基础上 ,重点对 2 0 0 1年 11月 14日昆仑山口西 8。
3) focal depth
震源深度
1.
The spatial and temporal distribution of focal depth before strong shocks in Yunnan;
云南地区强震前震源深度的时空展布
2.
A PTD method a new method for determinating focal depth and its application;
确定震源深度的PTD方法及其应用
3.
We used the catalog of Earthquake Administration of Xinjiang and HYPODD to analyze the characteristics of focal depth and its tectonic significance in Urumqi region,Xinjiang.
采用新疆维吾尔自治区地震局精度较高的常规地震目录和双差定位目录,对乌鲁木齐地区震源深度的分布特征及与断层的关系进行了研究。
4) Source depth
震源深度
1.
A method for numerical simulation of acoustic wave equation is used to simulate and analyze the characteristics of weathering propagation in seismic field for different source depthes.
采用声波波动方程数值模拟方法,对在不同震源深度情况下地震波场在低速带中的传播特征进行了模拟与分析。
2.
In this paper,based on a simple seismic model,a simple quantitative method to determine the boundary of potential seismic source is given according to two parameters of fault dips and source depth,and with concrete explanation of how to use the method.
基于简化地震模型， 根据发震断层的倾角、地震震源深度这两个参数， 提出一种简便的定量化确定潜在震源区边界的方法， 并对本方法的应用进行了具体说明。
3.
7, occurred in the circum-Pacific earthquake zone in June 1993, using PDE data and source depths of earthquakes from GDSN broadband data, this paper discusses the meanings of the source depth of earthquake preliminarily.
7级以上地震的分析，利用震中初始确定（PDE）资料及全球数字地震台网（GDSN）宽频带资料，对震源深度进行了初步讨论。
5) pool depth
余铁深度(炉)
6) Source depth of small earthquake
小震震源深度
补充资料：余震
见地震。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条