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In this paper,we use the data of JiaShi earthquake sequence which was recorded by KAS station and WUS station of the regional digital station network in XinJiang near source region. We have calculated moment tensor solutions of more than 100 Ms≥3.5 earthquakes from 2001 to 2004 by the body waveform inverse. At the same time,we compared our result with Harvard CMT result.

本文利用新疆区域数字化地震台网中近震源周围的喀什、乌什两个台记录到的伽师地震序列的波形资料,使用波形拟合反演方法分别计算了该区域2001-2004年的100余个Ms≥3.5地震的矩张量解,得到了一系列的震源参数。

There are two important questions: one is what is the properties of the seismicity before the earthquake, the other is about the character of the aftershock sequence.

两个重要的问题是,在这次地震之前,地震活动有什么样的性质;这次大地震的余震活动,具有怎样的特征。

Conversely, supermarine landslides and cosmic-body impacts disturb the water from above, as momentum from falling debris is transferred to the water into which the debris falls.

地震是发生在板块边缘的逆冲型地震,它所释放出的能量在近几十年来是较大的。逆冲型地震的成因是地层断层的上部上移。

Based on the pre-research of Reservior-Induced Seimicity, the text analyzed water's load effect, interstitial water pressure and chemicophysical effect on rock in Reservior-Induced Seimicity and discussed hydrogeological mechanism of Reservior-Induced Seimicity. The analysis supplys reliance for the hydrogeological analysis of Reservior-Induced Seimicity.

本文在总结水库诱发地震前人研究成果的基础上,系统分析了库水在水库诱发地震中的荷载效应,空隙水压力效应和对岩体的物理化学作用,从理论上讨论了水库诱发地震的水文地质机理,为水库诱发地震的水文地质分析提供依据。

Based on the pre-research of Reservior-Induced Seimicity, the text analyzed waters load effect, interstitial water pressure and chemicophysical effect on rock in Reservior-Induced Seimicity and discussed hydrogeological mechanism of Reservior-Induced Seimicity. The analysis supplys reliance for the hydrogeological analysis of Reservior-Induced Seimicity.

本文在总结水库诱发地震前人研究成果的基础上,系统分析了库水在水库诱发地震中的荷载效应,空隙水压力效应和对岩体的物理化学作用,从理论上讨论了水库诱发地震的水文地质机理,为水库诱发地震的水文地质分析提供依据。

In addition, coseismic Coulomb stress changes also have great influence on aftershocks distribution.

同时,由于鲜水断裂带不同断裂间的相互作用,发生地震的断裂在其相邻的断裂上产生同震库仑应力增加,使下次地震发生于其相邻的断裂上,这也可能是鲜水河断裂带地震沿带南北迁移的重要物理机制。

These characteristics are resulted from the interaction of different faults along this seismotectonic belt and the influences of coseismic Coulomb stress changes on active fault seismic potential.

鲜水河断裂带四次时间上连续发生的地震序列中,每一次地震都发生于受其先前发生的地震的影响而产生了同震库仑应力增加的断裂上(0.01~2.55bar)。

Two earthquakes of M S 6.0 and M S 5.8 occurred on Jan. 3,1994 and on Feb. 16,1994 in Gonghe county of Qinghai Province. The macroseismic epicenter of the Gonghe M S6.0 earthquake was at Hongqi village of Heka town, 7km south to the Tanggemu farm. The intensity at the epicenter was Ⅷ. 9 people were slightly injured during the event. The direct economic loss was 57.4486 million Yuan.

1994年1月3日、2月16日在青海省共和县发生6.0级和5.8级地震,6.0级地震的微观震中为36.07° N 、100.16° E ,宏观震中位于塘格木农场南部约7km 的河卡乡红旗村牧业点,震中烈度Ⅷ度;5.8级地震的微观震中为36.13° N 、100.17° E ,宏观震中位于塘格木农场北东约21km 处的沙珠玉乡上卡力岗村,震中烈度Ⅶ度1)。

Shear-wave splitting does not indicate potential earthquake locations, but analysis of local seismicity by Ragnar Stefánsson correctly predicted the small fault on which the stress-forecast earthquake occurred.

剪切波爆裂并不表示潜在的地震的位置,但Ragnar Stefansson对当地地震活动性的分析正确的预测应力预测的地震发生的小断层。

The major earthquake that struck Haiti Tuesday may have shocked a region unaccustomed to such temblors, but the devastating quake was not unusual in that it was caused by the same forces that generate earthquakes the world over.

星期二的大地震沉重地打击了海地,震憾了罕见这样地震的地区。不过,世界各地由同样的力量引发的这种灾难性地震并不罕见。

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