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PMC方法在江苏测震台网监测能力评估中的应用

立凯,  何奕成,  宫杰,  何浩宇,  秦磊,  霍祝青

立凯,何奕成,宫杰,何浩宇,秦磊,霍祝青,2023. PMC方法在江苏测震台网监测能力评估中的应用. 震灾防御技术,18(3):642−650. doi:10.11899/zzfy20230321. doi: 10.11899/zzfy20230321
引用本文: 立凯,何奕成,宫杰,何浩宇,秦磊,霍祝青,2023. PMC方法在江苏测震台网监测能力评估中的应用. 震灾防御技术,18(3):642−650. doi:10.11899/zzfy20230321. doi: 10.11899/zzfy20230321
Li Kai, He Yicheng, Gong Jie, He Haoyu, Qin Lei, Huo Zhuqing. Analysis of Monitoring Capability of Jiangsu Seismic Network Based on PMC Method[J]. Technology for Earthquake Disaster Prevention, 2023, 18(3): 642-650. doi: 10.11899/zzfy20230321
Citation: Li Kai, He Yicheng, Gong Jie, He Haoyu, Qin Lei, Huo Zhuqing. Analysis of Monitoring Capability of Jiangsu Seismic Network Based on PMC Method[J]. Technology for Earthquake Disaster Prevention, 2023, 18(3): 642-650. doi: 10.11899/zzfy20230321

PMC方法在江苏测震台网监测能力评估中的应用

doi: 10.11899/zzfy20230321
基金项目: 江苏省地震局青年基金(202101);中国地震局地震应急与信息青年重点任务(CEAEDEM202308);国家自然科学基金(41874051);中国地震局地震星火科技计划项目(XH23015 A);江苏省地震局科技创新团队(2022-03、2022-04)
详细信息
    作者简介:

    立凯,男,生于1985年。工程师。主要从事地震监测等工作。E-mail:83411367@qq.com

    通讯作者:

    何奕成,男,生于1991年。工程师。主要从事地震监测及地震波衰减与成像的相关工作。E-mail:hyckevin@mail.ustc.edu.cn

Analysis of Monitoring Capability of Jiangsu Seismic Network Based on PMC Method

  • 摘要: 江苏测震台网经近20年的高速发展,已拥有75个数字测震台站,针对江苏台网监测能力的评估需求,同时为进一步优化台网布局,提高江苏测震台网监测能力提供参考意见,本文使用基于概率的完整性震级方法,利用江苏台网2009—2021年正式编目观测报告数据,对江苏台网进行监测能力评估。研究结果表明,江苏台网监测能力较好的地区为北部连云港周边地区,监测能力达到了$ {M}_{\mathrm{L}}\geqslant 1.0 $;其次为南部南京、镇江、常州及周边地区,监测能力达到了$ {M}_{\mathrm{L}}\geqslant 1.5 $;监测能力较差的地区为中部地区及近海海域,监测能力达到了$ {M}_{\mathrm{L}}\geqslant 2.0 $。整个江苏台网基本实现了$ {M}_{\mathrm{L}}\geqslant 2.0 $的监测能力,周边地区及中部近海海域基本实现了$ {M}_{\mathrm{L}}\geqslant 2.5 $的监测能力。
  • 图  1  江苏及共享的邻省地震台站和2009—2021年震中分布

    Figure  1.  Distribution of seismic stations of Jiangsu and adjacent provinces and earthquakes occurred during 2009—2021

    图  2  连云港台单台监测概率分布

    Figure  2.  Probability diagram of single station monitoring of Lianyungang station

    图  3  盐城台单台监测概率分布

    Figure  3.  Probability diagram of single station monitoring of Yancheng station

    图  4  南京台单台监测概率分布

    Figure  4.  Probability diagram of single station monitoring of Nanjing station

    图  5  $ {P}_{\mathrm{E}} $与$ {M}_{\mathrm{P}} $空间分布

    Figure  5.  Composite detection probability $ {{P}}_{\mathrm{E}} $ distribution map and $ {{M}}_{\mathrm{P}} $ spatial distribution map

    表  1  江苏台网典型台站单台检测概率

    Table  1.   Statistical table of single station detection probability of typical stations of Jiangsu network

    台站名称/代码L/km
    (ML=1.0、PD=100%)
    ML/级
    (L=100 km、PD=100%)
    L/km
    (ML=3.0、PD=100%)
    ML/级
    (L=250 km、PD=100%)
    噪声级别台基
    类型
    常熟/CS401.61503.5Ⅱ石英砂岩
    常州/CZ—1.4150—Ⅲ混合花岗岩
    邳州/PZ—1.71503.8Ⅱ石英砂岩
    徐州/XZ—2.7150—Ⅰ灰岩
    东海/DH201.81503.5Ⅰ混合花岗岩
    赣榆/GAY301.41503.3Ⅰ混合岩
    高淳/GC301.61503.5Ⅰ紫红长石砂岩
    灌云/GUY502.01503.2Ⅰ花岗片麻岩
    镇江/ZJ—2.1150—Ⅱ砂岩
    江宁/JN—3.4903.5Ⅱ砂岩
    浦口/PK——50—Ⅲ灰岩
    靖江/JJ—3.120—Ⅲ石英砂岩
    金坛/JT—4.650—Ⅱ砂岩
    溧水/LIS202.11503.6Ⅱ片麻岩
    泗洪/SH—2.01503.3Ⅱ安山岩
    宿迁/SQ—2.41503.6Ⅱ安山凝灰岩
    —锡/WX201.71503.5Ⅱ石英砂岩
    新沂/XIY202.21503.3Ⅱ砂岩
    徐圩/XW202.41503.7Ⅱ花岗片麻岩
    盱眙/XY—1.91003.7Ⅰ灰岩
    大丰(井下)/DF————Ⅲ松散沉积层
    高邮(井下)/GY—3.920—Ⅱ松散沉积层
    海安(井下)/HA—3.230—Ⅱ松散沉积层
    淮安(井下)/HUA—2.5150—Ⅱ松散沉积层
    涟水(井下)/LIS——30—Ⅱ石英岩
    溧阳(井下)/LY102.0150—Ⅰ安山玄武岩
    南通(井下)/NT——10—Ⅱ石英砂岩
    沛县(井下)/PX—2.450—Ⅱ石英砂岩
    启东(井下)/QD————Ⅱ混合花岗岩
    如东(井下)/RD——50—Ⅱ灰岩
    射阳(井下)/SY——20—Ⅲ松散沉积层
    泰州(井下)/TZ—2.9130—Ⅲ沉积岩
    兴化(井下)/XH————Ⅲ混合花岗岩
    盐城(井下)/YC——60—Ⅱ松散沉积层
    阳光岛(井下)/YGD————Ⅱ基岩
    宝应(井下)/BY—3.140—Ⅱ石英砂岩
    昆山/KS—2.5150—Ⅲ灰岩
    六合/LH—2.7150—Ⅰ白云岩
    前三岛/QSD————Ⅱ片麻岩
    宜兴/YX—2.5150—Ⅰ砂岩
    南京/NJ2—1.91503.3Ⅱ安山玄武岩
    连云港/LYG401.71503.1Ⅰ片麻岩
    下载: 导出CSV
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  • 收稿日期:  2022-04-24
  • 刊出日期:  2023-08-31

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