| 新疆民丰县皮什盖-塔勒克勒格断裂带的第四纪活动特征 |
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| 引用本文： | 柏美祥.新疆民丰县皮什盖-塔勒克勒格断裂带的第四纪活动特征[J].内陆地震,2003,17(2):97-100. |
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| 作者姓名： | 柏美祥 |
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| 作者单位： | 新疆维吾尔自治区地震局,新疆,乌鲁木齐,830011 |
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| 摘 要： | 皮什盖-塔勒克勒格断裂将蓟县系逆掩于第四系之上，中更新世之前的西域变动显著，现今地震活动不强烈。其分支断裂帕西木断裂在中更新世之后，由正断层变为压性断层。
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| 关 键 词： | 第四纪活动断裂 不整合面 西域变动 民丰县 |
| 文章编号： | 1001-8956(2003)02-0097-04 |
QUATERNARY ACTIVITY CHARACTER OF PISHIGAI-TA-LEKELEGE FAULT ZONE IN MINFENG, XINJIANG |
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| BAI Mei-xiang.QUATERNARY ACTIVITY CHARACTER OF PISHIGAI-TA-LEKELEGE FAULT ZONE IN MINFENG, XINJIANG[J].Inland Earthquake,2003,17(2):97-100. |
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| Authors: | BAI Mei-xiang |
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| Abstract: | The Jixian System thrusts upon the Quaternary System along the Pishigai-Talekelege fault zone in Minfeng, Xinjiang. The Xiyu movement was outstanding before the Middle Pleistocene in this area, while at present the seimic activity is not strong. Its branched fault, the Paximu fault, has changed to compressive fault from tensional one after the Middle Pleistocene. |
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| Keywords: | Quaternary active fault Discordant surface Xiyu movement Minfeng |
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