徐州废黄河断裂带的空间展布与活动性研究

doi:10.3969/j.issn.0253-4967.2011.01.007

地震地质 ›› 2011, Vol. 33 ›› Issue (1): 67-78.DOI: 10.3969/j.issn.0253-4967.2011.01.007

徐州废黄河断裂带的空间展布与活动性研究

陈丁^1,2, 张景发¹, 朱鲁², 姜文亮¹, 路晓翠^1,2, 刘建达³, 李丽梅³, 张鹏³

1. 中国地震局地壳应力研究所, 北京 100085;
2. 山东科技大学, 青岛 266510;
3. 江苏省地震局地震工程研究院, 南京 210014

收稿日期:2010-11-08 修回日期:2011-01-28 出版日期:2011-04-29 发布日期:2011-12-18
作者简介:陈丁,男,1984年生,2008年毕业于山东科技大学地质工程专业,获学士学位,目前在中国地震局地壳应力研究所攻读硕士学位,主要从事遥感地质解译、重磁解译学习与研究,电话:15210958910,E-mail: chending_224@163.com。
基金资助:
中国地震局地壳应力研究所基本科研业务专项(ZDJ20071)与"徐州市新城区开发区活断层探测与地震危险性评价"项目共同资助。

SPATIAL DISTRIBUTION AND ACTIVITY OF XUZHOU FEI HUANGHE FAULT ZONE

CHEN Ding^1,2, ZHANG Jing-fa¹, ZHU Lu², JIANG Wen-liang¹, LU Xiao-cui^1,2, LIU Jian-da³, LI Li-mei³, ZHANG Peng³

1. Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China;
2. Shandong University of Science and Technology, Qingdao 266510, China;
3. Earthquake Administration of Jiangsu Province, Nanjing 210014, China

Received:2010-11-08 Revised:2011-01-28 Online:2011-04-29 Published:2011-12-18

摘要/Abstract

摘要：

文中利用遥感影像分析了徐州废黄河断裂带的空间展布及与邵楼断裂的交切关系,利用重磁资料研究了废黄河断裂带的深部几何结构及与郯庐断裂带西边界的交切关系。二阶布格重力异常小波变换细节图反映出徐州废黄河断裂带的深度为7～8km,而三阶和四阶重力异常细节图反映的深度分别为9～11km和15～18km。研究结果表明,废黄河断裂带向SE延伸至九顶附近,向下的切割深度约为 8～9km。NW向的废黄河断裂带截切邵楼断裂致使邵楼断裂构造线自东北向西南由N60°E转至N45°E。废黄河断裂带与郯庐断裂带不相交。废黄河断裂带属于前第四纪断裂,活动性较弱。

关键词: 废黄河断裂带, 遥感, 重磁, 历史地震, 徐州

Abstract:

Based on the remote sensing images interpretation,the spatial distribution of the Fei Huanghe(the ancient Yellow River)fault zone in Xuzhou area was studied and the intersection relationships between Fei Huanghe Fault and Shaolou Fault,and Tan-lu Fault were discussed in the paper.Besides,we researched the deep-seated geometric structure of Fei Huanghe Fault by studying the gravity-magnetic data,and discussed the intersection relationships with the west boundary of Tan-lu Fault. The cutting depth of Fei Huanghe Fault reflected by second order-wavelet transform detail of the Bouguer gravity anomalies is up to 7～8km.The depth reflected by the third order-wavelet and fourth order-wavelet transform detail of the Bouguer gravity anomalies is up to 9～11km and 15～18km,respectively.The results show that the Fei Huanghe Fault extends to Jiuding in southeast direction.The cutting depth is up to 8～9km.The NW-trending Fei Huanghe Fault cut the NE-trending Shaolou Fault,resulting in the change of the tectonic line of the latter from striking N 60°E to N 45°E.Moreover,the Fei Huanghe Fault didn't cut the Tanlu Fault.It is a pre-Quaternary Fault with weak activity.

Key words: Fei Huanghe Fault zone, remote sensing, gravity and magnetic anomaly, historical earthquake, Xuzhou

中图分类号:

P315.2

陈丁, 张景发, 朱鲁, 姜文亮, 路晓翠, 刘建达, 李丽梅, 张鹏. 徐州废黄河断裂带的空间展布与活动性研究[J]. 地震地质, 2011, 33(1): 67-78.

CHEN Ding, ZHANG Jing-fa, ZHU Lu, JIANG Wen-liang, LU Xiao-cui, LIU Jian-da, LI Li-mei, ZHANG Peng. SPATIAL DISTRIBUTION AND ACTIVITY OF XUZHOU FEI HUANGHE FAULT ZONE[J]. SEISMOLOGY AND GEOLOGY, 2011, 33(1): 67-78.

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徐州废黄河断裂带的空间展布与活动性研究

SPATIAL DISTRIBUTION AND ACTIVITY OF XUZHOU FEI HUANGHE FAULT ZONE

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