| 1954年甘肃山丹7(1/4)级地震史料补遗 |
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| 引用本文： | 罗浩,雷中生,何文贵,刘百篪,曹娜,袁道阳.1954年甘肃山丹7(1/4)级地震史料补遗[J].震灾防御技术,2010,5(2):185-198. |
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| 作者姓名： | 罗浩 雷中生 何文贵 刘百篪 曹娜 袁道阳 |
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| 作者单位： | 1. 中国地震局兰州地震研究所,兰州,730000;中国地震局地震预测研究所兰州创新基地,兰州,730000
2. 中国地震局兰州地震研究所,兰州,730000 |
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| 基金项目： | 国家自然科学基金，甘肃省地震局青年地震科学基金(2009259)资助.中国地震局兰州地震研究所论著号:LC 2010022 |
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| 摘 要： | 在归纳1954年山丹71/4级地震已有地震史料的基础上,根据新获得的朱允明(2006)《山丹地震考察笔记》的详细考察资料,按照《新中国地震烈度表》重新评定了本次地震中各考察点的地震烈度,重新绘制了该地震的等震线图。其中,极震区Ⅸ—Ⅹ度区长轴方向为北西向,呈扁椭圆形,长轴直径约40km;Ⅷ度区南西侧为山丹盆地,第四纪沉积较厚,地震烈度衰减缓慢,因此,Ⅷ度区等震线向南明显突出。1954年山丹71/4级地震极震区位于龙首山北缘断裂西段,大致与该断裂的包代河-黑头山段相吻合,综合分析认为,该段断裂是本次地震的主发震断层,而破喇嘛顶西缘断裂和毛湖洞断裂是重要的参与断裂。
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| 关 键 词： | 1954年山丹71/4级地震 地震史料 等震线 发震构造 |
| 收稿时间： | 2009/11/23 0:00:00 |
Addendum of Historical Records of Shandan, Gansu Province 7? Earthquake in 1954 |
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| Luo Hao,Lei Zhongsheng,He Wengui,Liu Baichi,Cao Na and Yuan Daoyang.Addendum of Historical Records of Shandan, Gansu Province 7? Earthquake in 1954[J].Technology for Earthquake Disaster Prevention,2010,5(2):185-198. |
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| Authors: | Luo Hao Lei Zhongsheng He Wengui Liu Baichi Cao Na and Yuan Daoyang |
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| Institution: | Luo Hao1,2),Lei Zhongsheng1),He Wengui1,Liu Baichi1,Cao Na1,2) and Yuan Daoyang1,2)1) Lanzhou Institute of Seismology,China Earthquake Administration,Lanzhou 730000,China 2) Lanzhou Base of Institute of Earthquake Science,China |
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| Abstract: | Based on the ＂Seismic Intensity Scale of China＂,the seismic intensity of Shandan 71/4 earthquake in 1954 is re-evaluated,and the earthquake isoseismal line graph is redrawn.After detailed study of the historical records of Shandan 71/4 earthquake in 1954,as well as the newly acquired,detailed investigative data of Zhu Yunming（2006） ＂the investigative notes of Shandan Earthquake＂.In our new isoseismal map,the meizoseismal area（Ⅸ—Ⅹ degree） appears flat oval,with long axis diameter of about 40km with NW direction.The Quaternary sedimentary in Shandan basin is relatively thick,which makes the isoseismal line of Ⅷ degree is extrusive to south obviously.The epicenter area of Shandan 71/4 earthquake in 1954 is located in western section of the Longshoushan northern margin fault,roughly in line with Baodai river—Heitou Mountain segment of this fault.The comprehensive analysis indicates that this fault is the main causative fault of Shandan 71/4 earthquake,while Polamading western margin fault and Maohudong Fault are also involved in and play important roles in the occurrence of the earthquake. |
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| Keywords: | Shandan MS71/4 earthquake in 1954 Historical earthquake records Isoseismal line Causative structure |
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