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1)  moderately strong swarm
中强震群
2)  Strong earthquake swarm
强震群
1.
Comparison and study on active tectonics environment of strong earthquake swarms;
强震群活动构造环境比较研究
2.
The article studies 9 strong earthquake swarms of with the magnitude M_S≥6.
对比研究了国内、外9次6级以上强震群,发现强震群序列具有强度大、频度高、中强余震频繁、余震衰减起伏大、持续时间长、中强震前小震活动显示平静的特点。
3)  strong swarm
强烈震群
4)  Jiashi strong earthquake swarm
伽师强震群
1.
Tomographic determination of the upper crustal structure in Jiashi strong earthquake swarm region—joint inversion of explosion and earthquake data;
伽师强震群区上地壳三维速度层析成像——人工爆破和天然地震的联合反演
2.
Focal mechanism of Jiashi strong earthquake swarm and characteristics of the regional stress field;
伽师强震群震源机制与区域应力场特征
3.
Using the system cluster of focus mechanism solutions for moderate-strong earthquakes and the stress field inversion of focal region in the Jiashi strong earthquake swarm from 1997 to 1998,main result as followed are obtained:(1) The Jiashi strong earthquake swarm is characterized mainly by strike-slip and normal fault.
利用1997-1998年伽师强震群中强地震震源机制系统聚类及震源区应力场反演,得到以下主要结果:(1)伽师强震群中强地震主要以走滑和正断层为主,伽师震源区主压应力方向为NNE或近NS向,与相邻的柯坪块体区域构造应力场方向不一致;伽师强震群的破裂面沿NEE方向,属左旋破裂;(2)4~5级中强地震应力场反演得到最大主压应力轴为NNE向,最小主压应力轴为NWW向,中等主应力轴倾角为65°,比较直立;(3)伽师强震群震源区应力场在强震前后经历了一系列变化。
5)  medium-strong earthquake
中强震
1.
We found that,the R value shows mid-long term anomaly before medium-strong earthquake in East China and Anhui area,but mid-long term anomaly in the 100 kilometers area around the Tanlu fault and the joint area of Jiangsu,Shandong,Anhui Provinces which was delimite.
结果发现,华东地区、安徽地区中强震前R值异常表现为中短期异常特征,郯庐断裂带100km范围内及本年度划定为危险区的苏鲁皖交界地区,R值异常表现为中长期异常特征。
6)  Mid-Strong Earthquake
中强地震
1.
This article deals with a study conducted about the relevance of seismic activities far and near before a mid-strong earthquake in Daxinganling earthquake belt and assists to determine the medium and long-term earthquake prediction.
本文通过对大兴安岭地震带中强地震前,远近地震活动的相关性进行研究,为大兴安岭地震带中长期地震预报进行判定。
补充资料:陪群公登箕山赋得群字
【诗文】:
许由去已远,冥莫见幽坟。世薄人不贵,兹山唯白云。
宁知三千岁,复有尧为君。时佐激颓俗,登箕挹清芬。
高节虽旦暮,邈与洪崖群。



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【出处】:
全唐诗:卷882-9
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