| 昆仑构造带强震活动的特点 |
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| 引用本文： | 王筱荣,王琼.昆仑构造带强震活动的特点[J].华南地震,2002,22(3):39-43. |
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| 作者姓名： | 王筱荣 王琼 |
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| 作者单位： | 新疆地震局,新疆 乌鲁木齐 830011 |
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| 摘 要： | 分析了昆仑构造带的强震活动后认为，昆仑地震带强震活动在时空分布上具有轮回性、等间距性及由西向东的迁移特点；昆仑地震带强震震级西弱东强，而强震发震频次西高东低；西昆仑构造带帕米尔结点的强震活动对大陆地震活跃幕有前兆意义。
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| 关 键 词： | 强震活动 昆仑构造带 时空分布 震级 地震活跃幕 |
| 文章编号： | 1001-8662(2002)03-0039-05 |
| 修稿时间： | 2002年5月15日 |
Seismicity feature of strong earthquakes in Kunlun tectonic belt |
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| WANG Xiao-rong,WANG Qiong.Seismicity feature of strong earthquakes in Kunlun tectonic belt[J].South China Journal of Seismology,2002,22(3):39-43. |
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| Authors: | WANG Xiao-rong WANG Qiong |
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| Abstract: | Based on the studies of the activity of strong earthquakes of Kunlun tectonic belt, we find that the activity of strong earthquakes in Kunlun shows the characteristics of recurrence in temporal and spatial distribution, equidistance and migration from east to west. The magnitude is larger in the east than that in the west, but the frequency is lower in east than that in the west. The strong earthquakes in the Pamirs' nodes of western Kunlun tectonic belt can be as significant precursors for mainland active episodes |
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| Keywords: | Strong earthquake Activity characteristics Kunlun tectonic belt |
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