Enhanced reservoir-induced earthquakes in Koyna region, India, during 1993-95

被引:33
作者
Gupta, HK [1 ]
Rastogi, BK [1 ]
Chadha, RK [1 ]
Mandal, P [1 ]
Sarma, CSP [1 ]
机构
[1] Natl Geophys Res Inst, Hyderabad 500007, Andhra Pradesh, India
关键词
D O I
10.1023/A:1009742428657
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Reservoir induced earthquakes began to occur in the vicinity of Shivajisagar Lake formed by Koyna Dam in Maharashtra state, western India, soon after its filling started in 1962. Induced earthquakes have continued to occur for the past 34 years in the vicinity of this reservoir, and so far a total of 10 earthquakes of M greater than or equal to 5.0, over 100 of M greater than or equal to 4 and about 100,000 of M greater than or equal to 0.0 have occurred. Every year, following the rainy season, the water level in the reservoir rises and induced earthquakes occur. Seismic activity during 1967-68 was most intense when globally, the largest reservoir induced earthquake occurred on 10 December, 1967. Other years of intense seismic activity are 1973 and 1980. During 1986 another reservoir, Warna, some 20 km south of Koyna, began to be filled. The recent burst of seismic activity in Koyna-Warna region began in August, 1993, and was monitored with a close network of digital and analog seismographs. During August, 1993-December, 1995, 1,272 shocks of magnitude greater than or equal to 2 were located, including two earthquakes of M 5.0 and M 5.4 on 8 December, 1993 and 1 February, 1994, respectively. Two parallel epicentral trends in NNE-SSW direction, one passing through Koyna and the other through Warna reservoir are delineated. The 1993 increase in seismicity has followed a loading of 44.15 m in Warna reservoir during 11 June, 1993 through August 4, 1993, with a maximum rate of filling being 16 m/week. The larger shocks have been found to be preceded by a precursory nucleation process.
引用
收藏
页码:47 / 53
页数:7
相关论文
共 16 条
[1]   FORESHOCK SEQUENCE OF THE 1992 LANDERS, CALIFORNIA, EARTHQUAKE AND ITS IMPLICATIONS FOR EARTHQUAKE NUCLEATION [J].
DODGE, DA ;
BEROZA, GC ;
ELLSWORTH, WL .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1995, 100 (B6) :9865-9880
[2]  
Gupta H. K., 1976, Dams and Earthquakes
[3]  
Gupta H.K., 1992, RESERVOIR INDUCED EA
[4]  
GUPTA HK, 1980, B SEISMOL SOC AM, V70, P1833
[5]  
GUPTA HK, 1983, B SEISMOL SOC AM, V73, P679
[6]   CONTINUED SEISMIC ACTIVITY AT KOYNA RESERVOIR SITE, INDIA [J].
GUPTA, HK ;
COMBS, J .
ENGINEERING GEOLOGY, 1976, 10 (2-4) :307-313
[7]  
GUPTA HK, 1972, B SEISMOL SOC AM, V62, P493
[8]  
GUPTA HK, 1972, B SEISMOL SOC AM, V62, P481
[9]  
ISHIDA M, 1978, B SEISMOL SOC AM, V68, P1265
[10]   CRUSTAL STRUCTURE FROM DEEP SEISMIC-SOUNDINGS ALONG THE KOYNA-II (KELSI-LONI) PROFILE IN THE DECCAN TRAP AREA, INDIA [J].
KAILA, KL ;
MURTY, PRK ;
RAO, VK ;
KHARETCHKO, GE .
TECTONOPHYSICS, 1981, 73 (04) :365-384