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ISSN 2096-7780 CN 10-1665/P

葛计划, 曹志磊, 孙军, 卢叶啸, 于磊, 程玲, 陶媛, 孙伯乐, 陆立, 周自强. 郯庐断裂带中南段跨断层短水准形变特征初步分析[J]. 地震科学进展 , 2022, (11): 513-523, 535. DOI: 10.19987/j.dzkxjz.2022-078
引用本文: 葛计划, 曹志磊, 孙军, 卢叶啸, 于磊, 程玲, 陶媛, 孙伯乐, 陆立, 周自强. 郯庐断裂带中南段跨断层短水准形变特征初步分析[J]. 地震科学进展 , 2022, (11): 513-523, 535. DOI: 10.19987/j.dzkxjz.2022-078
Ge Jihua, Cao Zhilei, Sun Jun, Lu Yexiao, Yu Lei, Cheng Ling, Tao Yuan, Sun Bole, Lu Li, Zhou Ziqiang. Preliminary analysis on the characteristics of short leveling deformation across faults in the central and southern part of Tan-Lu fault zone[J]. Progress in Earthquake Sciences, 2022, (11): 513-523, 535. DOI: 10.19987/j.dzkxjz.2022-078
Citation: Ge Jihua, Cao Zhilei, Sun Jun, Lu Yexiao, Yu Lei, Cheng Ling, Tao Yuan, Sun Bole, Lu Li, Zhou Ziqiang. Preliminary analysis on the characteristics of short leveling deformation across faults in the central and southern part of Tan-Lu fault zone[J]. Progress in Earthquake Sciences, 2022, (11): 513-523, 535. DOI: 10.19987/j.dzkxjz.2022-078

郯庐断裂带中南段跨断层短水准形变特征初步分析

Preliminary analysis on the characteristics of short leveling deformation across faults in the central and southern part of Tan-Lu fault zone

  • 摘要: 通过对郯庐断裂带中南段近20年的跨断层定点水准测量资料的处理与分析,初步总结了郯庐断裂带中南段断层垂直形变的时空活动特征。2000—2019年郯庐断裂带中南段断层垂直形变活动整体水平不高,平均合成速率为0.19 mm/a,但具有明显的分时活动特征。2000—2010年槐柏—宿迁段活动相对较大,新沂—临沂段活动相对较小,宿迁和新沂之间存在相对闭锁段;2011—2019年整体活动速率有所降低,但安丘测点活动速率相对2000—2011年增大明显。郯庐断裂带中南段的活动特征和近20年来该地区地震活动情况存在一定的对应关系。

     

    Abstract: Based on the processing and analysis of the fixed-point horizontal deformation data across the fault in the middle and southern part of the Tan-Lu fault zone in recent 20 years, this paper preliminarily analyzes the vertical deformation characteristics of the middle and southern section of the Tan-Lu fault. The research shows that the overall activity level of the middle and southern part of the Tan-Lu fault zone is not high, and the average combining rate is 0.19 mm/a. However, it has obvious characteristics of time-sharing activities: from 2000 to 2010, the activity in Huaibai-Suqian section was large, while the activity in Xinyi-Linyi section was relatively small. There was a relatively closed section between Suqian and Xinyi; The overall activity rate has decreased from 2011 to 2019, but the activity rate of Anqiu station has increased significantly compared with that of 2000 to 2011. There is a certain correspondence between the activitycharacteristics of the fault zone and the seismicity of the region in the past 20 years.

     

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