A discussion on the records of water level “precursors” in Well Shuozhou, Shanxi Province
A lot of slow fluctuations of water level have been observed in the original recording maps of subsurface fluid in Well Shuozhou, Shanxi Province. Some typical recording maps of the (precursors( are introduced in the paper and the features of the (precursors( recorded by the well are analyzed. The r...
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Published in | Acta seismologica sinica Vol. 15; no. 2; pp. 226 - 233 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
Beijing
Springer Nature B.V
01.03.2002
Institute of Geology, China Seismological Bureau, Beijing 100029, China%Seismological Bureau of Shanxi Province, Taiyuan 030002, China%Seismological Office of Shuocheng District, Shuozhou, Shanxi Province, Shuozhou 038500, China |
Subjects | |
Online Access | Get full text |
ISSN | 1000-9116 1674-4519 1993-1344 1867-8777 |
DOI | 10.1007/s11589-002-0012-3 |
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Abstract | A lot of slow fluctuations of water level have been observed in the original recording maps of subsurface fluid in Well Shuozhou, Shanxi Province. Some typical recording maps of the (precursors( are introduced in the paper and the features of the (precursors( recorded by the well are analyzed. The results show that 38% strong earthquakes possess this kind of record, which has a fluctuation period arranging from several to tens of minutes and appear mostly two days before the earthquakes. Moreover, the mechanism, transmission and responding conditions of well water level are discussed, as well as the scientific meaning and practical value of the (precursor( of the well water level in earthquake predictions. |
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AbstractList | A lot of slow fluctuations of water level have been observed in the original recording maps of subsurface fluid in Well Shuozhou, Shanxi Province. Some typical recording maps of the (precursors( are introduced in the paper and the features of the (precursors( recorded by the well are analyzed. The results show that 38% strong earthquakes possess this kind of record, which has a fluctuation period arranging from several to tens of minutes and appear mostly two days before the earthquakes. Moreover, the mechanism, transmission and responding conditions of well water level are discussed, as well as the scientific meaning and practical value of the (precursor( of the well water level in earthquake predictions. A lot of slow fluctuations of water level have been observed in the original recording maps of subsurface fluid in Well Shuozhou, Shanxi Province. Some typical recording maps of the "precursors" are introduced in the paper and the features of the "precursors" recorded by the well are analyzed. The results show that 38% strong earthquakes possess this kind of record, which has a fluctuation period arranging from several to tens of minutes and appear mostly two days before the earthquakes. Moreover, the mechanism, transmission and responding conditions of well water level are discussed, as well as the scientific meaning and practical value of the "precursor" of the well water level in earthquake predictions.[PUBLICATION ABSTRACT] P315.72+3; A lot of slow fluctuations of water level have been observed in the original recording maps of subsurface fluid in Well Shuozhou, Shanxi Province. Some typical recording maps of the (precursors( are introduced in the paper and the features of the (precursors( recorded by the well are analyzed. The results show that 38% strong earthquakes possess this kind of record, which has a fluctuation period arranging from several to tens of minutes and appear mostly two days before the earthquakes. Moreover, the mechanism, transmission and responding conditions of well water level are discussed, as well as the scientific meaning and practical value of the (precursor( of the well water level in earthquake predictions. |
Author | CHE Yong-tai (车用太) YU Jin-zi (鱼金子) ZHANG Shu-liang (张淑亮) FAN Xue-fang (范雪芳) GUO Jun-jie (郭君杰) ZHANG Tian-yuan (张天原) YANG Jin-lan (杨金兰) |
AuthorAffiliation | Institute of Geology, China Seismological Bureau, Beijing 100029, China Institute of Geology, China Seismological Bureau, Beijing 100029, China Seismological Bureau of Shanxi Province, Taiyuan 030002, China Seismological Bureau of Shanxi Province, Taiyuan 030002, China Seismological Bureau of Shanxi Province, Taiyuan 030002, China Seismological Office of Shuocheng District, Shuozhou, Shanxi Province, Shuozhou 038500, China Seismological Office of Shuocheng District, Shuozhou, Shanxi Province, Shuozhou 038500, China |
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Cites_doi | 10.1029/JZ070i016p03915 10.2307/3978420 10.1126/science.248.4962.1490 10.1029/91GL02414 |
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Snippet | A lot of slow fluctuations of water level have been observed in the original recording maps of subsurface fluid in Well Shuozhou, Shanxi Province. Some typical... P315.72+3; A lot of slow fluctuations of water level have been observed in the original recording maps of subsurface fluid in Well Shuozhou, Shanxi Province.... |
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SubjectTerms | Earthquake prediction Earthquakes Fluctuation Fluid dynamics level precursor Precursors Recording Seismic activity Seismic phenomena Shuozhou water Water levels well Well water Well waters |
Title | A discussion on the records of water level “precursors” in Well Shuozhou, Shanxi Province |
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