zhenbo

ISSN 2096-7780 CN 10-1665/P

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

2019年四川长宁MS6.0地震前破裂区内视应力和b值的变化

陈学忠 李艳娥 宫悦 陈丽娟

陈学忠, 李艳娥, 宫悦, 陈丽娟. 2019年四川长宁MS6.0地震前破裂区内视应力和b值的变化[J]. 地震科学进展, 2021, (2): 49-58. doi: 10.3969/j.issn.2096-7780.2021.02.001
引用本文: 陈学忠, 李艳娥, 宫悦, 陈丽娟. 2019年四川长宁MS6.0地震前破裂区内视应力和b值的变化[J]. 地震科学进展, 2021, (2): 49-58. doi: 10.3969/j.issn.2096-7780.2021.02.001
Xuezhong Chen, Yan’e Li, Yue Gong, Lijuan Chen. Variations in apparent stress and b value in the rupture area before the 2019 MS6.0 Changning earthquake[J]. Progress in Earthquake Sciences, 2021, (2): 49-58. doi: 10.3969/j.issn.2096-7780.2021.02.001
Citation: Xuezhong Chen, Yan’e Li, Yue Gong, Lijuan Chen. Variations in apparent stress and b value in the rupture area before the 2019 MS6.0 Changning earthquake[J]. Progress in Earthquake Sciences, 2021, (2): 49-58. doi: 10.3969/j.issn.2096-7780.2021.02.001

2019年四川长宁MS6.0地震前破裂区内视应力和b值的变化

doi: 10.3969/j.issn.2096-7780.2021.02.001
基金项目: 国家重点研发计划(2018YFC1503405)资助。
详细信息
    通讯作者:

    陈学忠(1963-),男,研究员,主要从事地震学与地震预测研究。E-mail:cxz8675@163.com

  • 中图分类号: P315.72+7

Variations in apparent stress and b value in the rupture area before the 2019 MS6.0 Changning earthquake

  • 摘要: 视应力和b值都可以反映地壳应力变化。当应力增加时,视应力会增加,而b值降低。因此,应力变化将导致视应力和b值之间呈负相关关系,即,根据视应力和b值之间的负相关关系可以研究地壳构造应力的变化。本文利用2000年1月—2019年12月长宁MS6.0地震破裂区内3.0≤ML≤3.6地震的视应力和2.0≤ML≤4.3地震目录,研究了视应力和b值随时间的变化,发现:2013年2月—2017年3月间,视应力呈趋势上升变化,历时约4年,在震前两年时间内,视应力仍维持在较高水平。在视应力呈趋势上升变化期间,b值则呈趋势下降变化。当视应力维持在较高水平时,b值则维持在较低水平。即,长宁MS6.0地震发生前,破裂区内视应力增加,同时b值下降。这表明,2019年长宁MS6.0地震发生前破裂区内存在明显的构造应力增加过程,对地震孕育过程的认识和地震预测研究都具有启示意义。

     

  • 图  1  (a)长宁地震余震空间分布(2019年6月17日—7月31日,ML≥0.0)以及全球质心矩张量解(沙滩球,箭头表示断层面错动方向); (b)长宁地震以及历史上发生的MS≥6.0地震(“○”)。F1:华蓉山断裂带;F2:马边—盐津断裂带;F3:莲峰断裂带;F4:峨边—金阳断裂带。 “☆”为长宁地震震中

    Figure  1.  (a)Spatial distribution of epicenters of ML≥ 0.0 aftershocks that occurred from June 17,2019 to July 31,2019 and the GCMT solution for the June 17,2019 Changning MS6.0 earthquake(beach ball,arrows indicate the slipping direction of the focal fault) . F1 indicates the Huarongshan fault;F2 indicates the Mabian-Yanjin fault;F3 indicates the Lianfeng fault and F4 indicates the Ebian-Jinyang fault. The star shows the epicenter of the Changning earthquake

    图  2  视应力与震级的关系

    Figure  2.  Apparent stress versus magnitude

    图  3  研究区内ML≥1.0地震震级随时间变化

    Figure  3.  Magnitude versus time for earthquakes(ML≥1.0)that occurred in the study area

    图  4  不同时期地震的G-R关系

    Figure  4.  The G-R relation of earthquakes in different periods

    图  5  视应力随时间的变化

    (a)以20个地震计算平均值,2个地震滑动; (b)以30个地震计算平均值,2个地震滑动

    Figure  5.  Apparent stress as a function of time

    (a)20-event mean,shifted by two events per time; (b)30-event mean,shifted by two events per time

    图  6  b值(黑色实线)随时间的变化。以400次地震为滑动窗口计算b值,20次地震滑动。 “↓”标注长宁MS6.0地震发生时间。 “○”为视应力的30个事件平均值

    Figure  6.  b value(the black solid line)as a function of time obtained by applying a sliding time window of 400 events moved by 20 events. The down arrow“↓” shows the original time of the Changning MS6.0 main event. The circle “○” denotes the 30-event mean of the apparent stress

    表  1  地震矩、地震能量和视应力计算结果

    Table  1.   Calculated seismic moment,seismic energy and apparent stress for the studied earthquakes

    序号年-月-日纬度/°N经度/°WML地震矩/(×1015 N•m)Es/(×1011 N•m)σapp/bar
    12002-04-2928.42104.703.81.700000.049400.82
    22003-03-0828.37104.803.20.315000.009920.97
    32003-06-2328.47104.803.40.365000.006150.45
    42005-02-0528.32104.933.20.197000.004750.57
    52005-12-1928.27104.973.50.468000.015100.88
    62006-04-0228.37105.023.40.282000.004630.36
    72006-04-2828.38104.883.00.149000.003030.36
    82006-07-1228.37104.883.00.097800.000660.18
    92006-08-0128.33104.983.92.220000.173001.69
    102006-08-0128.27104.984.03.010000.242002.09
    112006-08-2528.38104.853.00.097700.000400.12
    122006-08-2728.35104.973.00.198000.006140.56
    132006-10-3028.33104.923.30.289000.004980.42
    142006-10-0228.33104.903.10.196000.003380.42
    152006-10-3028.33104.923.30.291000.005000.41
    162006-11-2428.30104.923.00.170000.001830.26
    172007-01-0428.37104.953.81.130000.086001.83
    182007-01-1128.33104.873.40.479000.017400.81
    192007-01-2728.35105.033.40.437000.014000.65
    202007-03-1228.37104.983.40.348000.005410.36
    212007-04-2228.32104.923.60.651000.026100.93
    222007-04-2328.35104.903.40.401000.011900.70
    232007-04-2428.40105.003.30.529000.013300.58
    242007-04-2528.33104.953.60.632000.024400.92
    252007-05-0828.33105.003.40.439000.011400.73
    262007-05-1028.30104.933.00.108000.000960.21
    272007-05-3128.33104.983.20.222000.004510.38
    282007-06-1828.35104.853.91.320000.136002.10
    292007-06-1928.32104.953.20.192000.003240.35
    302007-06-1928.30104.953.10.161000.001390.23
    312007-06-1928.28104.953.80.720000.040401.32
    322007-08-0828.30104.953.60.948000.066201.54
    332007-08-1428.30104.924.12.500000.347003.53
    342007-08-1428.30104.923.60.522000.025701.19
    352007-08-1628.30104.903.81.120000.080001.88
    362007-08-2928.50104.773.20.130000.000970.19
    372007-09-1328.32104.883.20.179000.002830.38
    382007-09-1728.30104.903.10.169000.002600.37
    392007-09-2228.33104.883.10.259000.004330.39
    402007-10-0628.33104.984.22.380000.337003.21
    412007-10-1028.33104.923.10.095000.000760.26
    422007-10-1228.37104.883.40.141000.002160.43
    432007-10-2228.38104.883.40.156000.001530.31
    442007-10-2228.37104.873.20.082600.000620.23
    452007-10-2428.37104.883.20.094600.000990.29
    462007-10-2428.38104.883.40.096300.000960.28
    472007-11-0128.38104.873.00.061900.000430.19
    482007-11-1128.38104.883.90.766000.026000.91
    492007-11-1128.37104.883.30.150000.001650.33
    502008-02-0128.33104.884.86.090001.310005.82
    512008-02-0228.38104.953.20.113000.001360.34
    522008-02-0528.37104.853.20.072500.000680.28
    532008-02-0528.38104.883.20.116000.001060.27
    542008-02-1428.37104.833.80.477000.017200.94
    552008-02-1428.37104.833.30.148000.001410.26
    562008-02-2028.48104.733.40.140000.001690.30
    572008-07-1928.35104.923.00.096000.000850.25
    582008-08-2928.37104.883.80.211000.004410.60
    592009-01-0128.37104.853.50.242000.005590.48
    602009-06-1028.33104.883.40.335000.009710.78
    612009-06-1228.35104.833.00.086400.000610.16
    622009-11-2728.37104.883.00.082400.000890.31
    632010-03-2628.37104.883.10.069900.000550.21
    642010-07-1628.42104.884.00.721000.051102.04
    652010-08-2528.37104.883.00.052100.000310.18
    662010-10-0128.37104.903.20.124000.001530.28
    672010-10-0628.37104.924.63.240000.880007.42
    682010-10-2428.37104.883.20.118000.002120.51
    692010-12-0328.32104.923.71.630000.210003.15
    702011-04-3028.37104.923.80.725000.057802.09
    712011-04-3028.35104.923.40.376000.016001.03
    722011-06-0228.33104.923.91.050000.087402.19
    732011-06-2628.37104.924.31.790000.188002.78
    742011-10-0528.35104.883.30.179000.001950.31
    752012-04-0928.38104.934.11.430000.138002.41
    762012-07-2628.38104.833.00.087000.001090.41
    772012-07-2828.42104.834.00.748000.047201.78
    782012-07-2928.38104.833.40.214000.005590.78
    792012-07-3128.38104.853.50.259000.004600.52
    802012-07-3128.40104.833.10.085100.000630.22
    812012-08-0728.42104.833.30.120000.001990.50
    822012-08-1328.38104.833.30.151000.003070.61
    832012-10-1928.35104.883.20.137000.002300.45
    842013-02-1228.32104.873.10.148000.002260.32
    852013-02-1928.30104.904.55.760002.5400010.81
    862013-02-2728.33104.883.10.130000.001650.28
    872013-04-2528.40104.905.213.500007.2100016.14
    882013-04-2528.40104.904.76.430001.470006.29
    892013-04-2528.40104.803.70.514000.033501.63
    902013-05-0728.35104.874.01.040000.087802.64
    912013-07-1728.33104.883.70.493000.021501.24
    922013-10-0928.38104.903.40.285000.005880.53
    932013-10-0928.37104.903.30.292000.008980.74
    942013-11-2628.37104.903.10.143000.001510.32
    952014-01-1428.33104.933.60.430000.015600.96
    962014-05-0828.33104.923.30.170000.003560.64
    972014-05-2028.37104.923.20.195000.002630.38
    982014-07-1828.42104.873.30.181000.003410.48
    992014-07-2028.42104.873.00.103000.001360.37
    1002014-08-2428.40104.873.30.172000.004210.67
    1012015-01-2828.38104.883.20.158000.001900.33
    1022015-01-2828.37104.953.90.985000.049801.35
    1032015-02-0728.37104.904.89.060004.2300012.60
    1042015-02-0728.37104.903.80.791000.039101.38
    1052015-02-0828.37104.873.60.361000.008250.67
    1062015-03-2528.42104.823.60.266000.009020.94
    1072015-06-2628.42104.803.00.071800.000940.36
    1082015-08-2728.35104.883.00.101000.001430.41
    1092015-10-1328.37104.903.00.097500.000920.28
    1102015-11-3028.37104.974.01.150000.132002.18
    1112016-04-1928.38104.933.40.136170.009661.13
    1122016-05-0628.40104.823.40.184850.012181.16
    1132016-05-0628.32104.873.10.095560.002800.54
    1142016-05-1328.42104.823.30.127550.006120.83
    1152016-06-0828.43104.803.70.440570.029461.46
    1162016-09-2928.37104.773.10.160270.001400.25
    1172017-01-1028.38104.873.40.173830.011891.18
    1182017-03-2428.40104.923.00.054970.001800.51
    1192017-09-2128.37104.923.10.073220.000440.15
    1202017-09-2628.35104.923.20.074150.001290.34
    1212017-10-0728.33104.923.00.050870.000780.28
    1222018-05-0428.39104.783.40.114290.006550.91
    1232018-05-0528.38104.784.10.849660.072712.07
    1242018-07-2028.38104.773.00.054710.000740.26
    1252019-01-0428.37104.933.80.602310.019940.99
    1262019-01-1128.37104.933.20.109250.002010.55
    1272019-06-2528.42104.793.50.170940.005240.92
    1282019-06-2628.39104.813.90.447490.021301.43
    1292019-06-2728.43104.803.90.448410.035502.38
    1302019-06-2728.40104.803.50.197870.006921.05
    1312019-06-2928.43104.763.90.422870.027851.98
    1322019-06-3028.43104.773.50.183700.004500.73
    1332019-06-3028.44104.813.70.249110.015141.82
    1342019-09-0628.44104.804.21.457100.191223.94
    1352019-09-1228.43104.754.21.476200.119412.43
    1362019-10-0828.42104.783.10.052540.000640.36
    1372019-10-1128.38104.883.00.032820.000310.28
    1382019-10-1128.38104.873.20.067460.000890.40
    1392019-10-1428.38104.873.00.033070.000200.19
    1402019-10-1728.42104.783.20.061830.001010.49
    1412019-10-1928.35104.873.10.112210.001070.29
    1422019-10-1928.43104.723.50.117580.004401.12
    1432019-10-2128.37104.934.11.318200.077211.76
    1442019-10-2728.40104.823.10.077970.000600.23
    1452019-11-0228.43104.683.30.165230.001550.28
    1462019-11-0528.43104.823.10.066250.000420.19
    1472019-11-0728.37104.973.80.393470.016731.27
    1482019-11-1028.45104.783.00.048240.000290.18
    1492019-11-1028.43104.733.90.375090.019341.55
    1502019-11-1428.38104.933.60.214610.004840.68
    1512019-11-1428.38104.953.00.029710.000140.14
    1522019-11-2128.45104.773.20.063710.000540.25
    1532019-11-2728.37104.934.31.541600.124282.42
    1542019-12-2328.43104.773.40.116170.001930.50
    1552019-12-2628.43104.823.80.420820.008920.64
    1562019-12-2928.38104.934.10.656870.026211.20
    下载: 导出CSV
  • [1] Madariaga R. Dynamics of an expanding circular fault[J]. Bull. Seismol. Soc. Amer.,1976,66(3):639-666
    [2] Das S,Aki K. Fault plane with barriers:A versatile earthquake model[J]. J. Geophys. Res.,1977,82(36):5658-5670 doi: 10.1029/JB082i036p05658
    [3] Aki K. Characterization of barriers on an earthquake fault[J]. J. Geophys. Res.,1979,84(B11):6140-6148 doi: 10.1029/JB084iB11p06140
    [4] Aki K. Asperities,barriers,characteristic earthquakes and strong motion prediction[J]. J. Geophys. Res,1984,89(NB7):5867-5872 doi: 10.1029/JB089iB07p05867
    [5] Fedotov S A,Gusev A A,Boldyrev S A. Progress of earthquake prediction in Kamchatka[J]. Tectonophysics,1972,14(3/4):279-286
    [6] Tsujiura M. Spectral features of foreshocks[J]. Bull. Earthquake Res. Inst. Univ. Tokyo,1977,52:357-371
    [7] Bakun W H,McEvilly T V. Are foreshocks distinctive? Evidence from the 1966 Parkfield and the 1975 Oroville,California sequences[J]. Bull. Seismol. Soc. Amer.,1979,69(4):1027-1038
    [8] Bakun W H,McEvilly T V. P-wave spectra for ML5 foreshocks,aftershocks and isolated earthquakes near Parkfield,California[J]. Bull. Seismol. Soc. Amer,1981,71(2):423-436
    [9] Ishida M,Kanamori H. Temporal variation of seismicity and spectrum of small earthquakes preceding the 1952 Kern County,California,earthquake[J]. Bull. Seismol. Soc. Amer,1980,70(2):509-527
    [10] Wyss M. Apparent stresses of earthquakes on ridges compared to apparent stresses of earthquakes in trenches[J]. Geophys. J. Int.,1970,19(5):479-484 doi: 10.1111/j.1365-246X.1970.tb00153.x
    [11] Zobin V M. Apparent stress of earthquakes within the shallow subduction zone near Kamchatka Peninsula[J]. Bull. Seismol. Soc. Amer.,1996,86(3):811-820
    [12] Frank S,Carl K. Variations of apparent stresses and stress drops prior to the earthquake of 6 May 1984 (mb=5.8)in the Adak seismic zone[J]. Bull. Seismol. Soc. Amer.,1984,74(6):577-2592
    [13] 李艳娥,陈学忠,王恒信. 汶川8.0级地震前四川地区地震视应力时空变化特征[J]. 地震,2012,32(4):113-122 doi: 10.3969/j.issn.1000-3274.2012.04.012

    Li Yan’e,Chen Xuezhong,Wang Hengxin. Temporal and spatial variation of apparent stress in Sichuan area before the MS8.0 Wenchuan earthquake[J]. Earthquake,2012,32(4):113-122 doi: 10.3969/j.issn.1000-3274.2012.04.012
    [14] 李艳娥,陈学忠. 2011年日本MW9.1地震前后破裂区内视应力时空变化[J]. 地震,2017,37(4):10-21 doi: 10.3969/j.issn.1000-3274.2017.04.002

    Li Yan’e,Chen Xuezhong. Temporal and spacial variations of apparent stress in the rupture volume before and after the 2011 Tohoku,Japan,MW9.1 earthquake[J]. Earthquake,2017,37(4):10-21 doi: 10.3969/j.issn.1000-3274.2017.04.002
    [15] Zúñiga F R,Wyss M,Wilson M E. Apparent stresses,stress drops,and amplitude ratios of earthquakes preceding and following the 1975 Hawaii MS=7.2 main shock[J]. Bull. Seismol. Soc. Amer.,1987,77(1):69-96
    [16] Picozzi M,Bindi D,Zollo A,et al. Detecting long-lasting transients of earthquake activity on a fault system by monitoring apparent stress,ground motion and clustering[J]. Scientific Reports,2019,9:1-11 doi: 10.1038/s41598-018-37186-2
    [17] Calderoni G,Rovelli A,Giovambattista R D. Stress drop,apparent stress,and radiation efficiency of clustered earthquakes in the nucleation volume of the 6 April 2009,MW6.1 L’Aquila earthquake[J]. J. Geophys. Res.,2019,124(10):10360-10375
    [18] Mogi K. Magnitude-frequency relations for elastic shocks accompanying fracture of various materials and some related problems in earthquakes[J]. Bull. Earthquake Res. Inst. Univ. Tokyo,1962,40(4):851-853
    [19] Scholz C H. The frequency-magnitude relation of microfracturing in rock and its relation to earthquakes[J]. Bull. Seismol. Soc. Amer.,1968,58(1):399-415
    [20] Scholz C H. Microfractures,aftershocks,and seismicity[J]. Bull. Seismol. Soc. Amer.,1968,58(3):1117-1130
    [21] Wyss M. Towards a physical understanding of the earthquake frequency distribution[J]. Geophys. J. Int.,1973,31(4):341-359 doi: 10.1111/j.1365-246X.1973.tb06506.x
    [22] Main I G,Meredith P,Jones C. A reinterpretation of the precursory seismic b-value anomaly from fracture mechanics[J]. Geophys. J. Int.,1989,96(1):131-138 doi: 10.1111/j.1365-246X.1989.tb05255.x
    [23] Urbancic T I,Trifu C I,Long J M,et al. Space-time correlations of b values with stress release[J]. Pure Appl. Geophys.,1992,139:449-462 doi: 10.1007/BF00879946
    [24] Hainzl S,Zöller G,Kurths J. Similar power laws for foreshock and aftershock sequences in a spring-block model for earthquakes[J]. J. Geophys. Res.,1999,104:7243-7253 doi: 10.1029/1998JB900122
    [25] Nuannin P,Kulhanek O,Persson L. Spatial and temporal b value anomalies preceding the devastating off coast of NW Sumatra earthquake of December 26,2004[J]. Geophys. Res. Lett.,2005,32(11):L11307 doi: 10.1029/2005GL022679
    [26] Imoto M. Changes in the magnitude-frequency b-value prior to large (M=6.0)earthquakes in Japan[J]. Tectonophysics,1991,193(4):311-325 doi: 10.1016/0040-1951(91)90340-X
    [27] Chan C H,Wu Y M,Tseng T L,et al. Spatial and temporal evolution of b-values before large earthquakes in Taiwan[J]. Tectonophysics,2012,532-535:215-222
    [28] Enescu B,Ito K. Some premonitory phenomena of the 1995 Hyogo-Ken Nanbu (Kobe)earthquake:Seismicity,b-value and fractal dimension[J]. Tectonophysics,2001,338(3):297-314
    [29] Nanjo K Z,Hirata N,Obara K,et al. Decade-scale decrease in b value prior to the M9-class 2011 Tohoku and 2004 Sumatra quakes[J]. Geophys. Res. Lett.,2012,39(20):L20304
    [30] Aki K. Maximum likelihood estimate of b in the formula log N=a-bM and its confidence limits[J]. Bull. Earthquake Res. Inst. Univ. Tokyo,1965,43:237-239
    [31] Savage J C,Wood M D. The relation between apparent stress and stress drop[J]. Bull. Seismol. Soc. Amer.,1971,61(5):1381-1388
    [32] 秦保燕,姚立珣,李亚荣. 大震前震源外围区高b值震群产生的一种物理机制[J]. 地震,1983,3(6):6-11

    Qin Baoyan,Yao Lixun,Li Yarong. Physical mechanism of earthquake clusters with high b value in the periphery area of the focal source before major earthquakes[J]. Earthquake,1983,3(6):6-11
  • 加载中
图(6) / 表(1)
计量
  • 文章访问数:  376
  • HTML全文浏览量:  73
  • PDF下载量:  49
出版历程
  • 收稿日期:  2020-09-24
  • 修回日期:  2020-09-28
  • 网络出版日期:  2021-03-02
  • 刊出日期:  2021-02-25

目录

    /

    返回文章
    返回
    本系统由北京仁和汇智信息技术有限公司设计开发 百度统计