Tectonically Induced Anomalies Without Large Earthquake Occurrences
In this study, we documented a case involving large-scale macroscopic anomalies in the Xichang area, southwestern Sichuan Province, China, from May to June of 2002, after which no major earthquake occurred. During our field survey in 2002, we found that the timing of the high-frequency occurrence of...
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Veröffentlicht in: | Pure and applied geophysics 2018-07, Vol.175 (7), p.2513-2526 |
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description | In this study, we documented a case involving large-scale macroscopic anomalies in the Xichang area, southwestern Sichuan Province, China, from May to June of 2002, after which no major earthquake occurred. During our field survey in 2002, we found that the timing of the high-frequency occurrence of groundwater anomalies was in good agreement with those of animal anomalies. Spatially, the groundwater and animal anomalies were distributed along the Anninghe–Zemuhe fault zone. Furthermore, the groundwater level was elevated in the northwest part of the Zemuhe fault and depressed in the southeast part of the Zemuhe fault zone, with a border somewhere between Puge and Ningnan Counties. Combined with microscopic groundwater, geodetic and seismic activity data, we infer that the anomalies in the Xichang area were the result of increasing tectonic activity in the Sichuan–Yunnan block. In addition, groundwater data may be used as a good indicator of tectonic activity. This case tells us that there is no direct relationship between an earthquake and these anomalies. In most cases, the vast majority of the anomalies, including microscopic and macroscopic anomalies, are caused by tectonic activity. That is, these anomalies could occur under the effects of tectonic activity, but they do not necessarily relate to the occurrence of earthquakes. |
doi_str_mv | 10.1007/s00024-017-1596-9 |
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During our field survey in 2002, we found that the timing of the high-frequency occurrence of groundwater anomalies was in good agreement with those of animal anomalies. Spatially, the groundwater and animal anomalies were distributed along the Anninghe–Zemuhe fault zone. Furthermore, the groundwater level was elevated in the northwest part of the Zemuhe fault and depressed in the southeast part of the Zemuhe fault zone, with a border somewhere between Puge and Ningnan Counties. Combined with microscopic groundwater, geodetic and seismic activity data, we infer that the anomalies in the Xichang area were the result of increasing tectonic activity in the Sichuan–Yunnan block. In addition, groundwater data may be used as a good indicator of tectonic activity. This case tells us that there is no direct relationship between an earthquake and these anomalies. In most cases, the vast majority of the anomalies, including microscopic and macroscopic anomalies, are caused by tectonic activity. That is, these anomalies could occur under the effects of tectonic activity, but they do not necessarily relate to the occurrence of earthquakes.</description><identifier>ISSN: 0033-4553</identifier><identifier>EISSN: 1420-9136</identifier><identifier>DOI: 10.1007/s00024-017-1596-9</identifier><language>eng</language><publisher>Cham: Springer International Publishing</publisher><subject>Anomalies ; Earth and Environmental Science ; Earth Sciences ; Earthquakes ; Fault zones ; Geophysics/Geodesy ; Groundwater ; Groundwater data ; Groundwater levels ; Hydrologic data ; Rock deformation ; Seismic activity ; Surveying ; Tectonics</subject><ispartof>Pure and applied geophysics, 2018-07, Vol.175 (7), p.2513-2526</ispartof><rights>Springer International Publishing AG 2017</rights><rights>Pure and Applied Geophysics is a copyright of Springer, (2017). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a339t-529b13243c094997c0b990b14666e4240a8a4cc32e6e23ac86a245a2c5705cde3</citedby><cites>FETCH-LOGICAL-a339t-529b13243c094997c0b990b14666e4240a8a4cc32e6e23ac86a245a2c5705cde3</cites><orcidid>0000-0002-9827-9008</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s00024-017-1596-9$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00024-017-1596-9$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Shi, Zheming</creatorcontrib><creatorcontrib>Wang, Guangcai</creatorcontrib><creatorcontrib>Liu, Chenglong</creatorcontrib><creatorcontrib>Che, Yongtai</creatorcontrib><title>Tectonically Induced Anomalies Without Large Earthquake Occurrences</title><title>Pure and applied geophysics</title><addtitle>Pure Appl. Geophys</addtitle><description>In this study, we documented a case involving large-scale macroscopic anomalies in the Xichang area, southwestern Sichuan Province, China, from May to June of 2002, after which no major earthquake occurred. During our field survey in 2002, we found that the timing of the high-frequency occurrence of groundwater anomalies was in good agreement with those of animal anomalies. Spatially, the groundwater and animal anomalies were distributed along the Anninghe–Zemuhe fault zone. Furthermore, the groundwater level was elevated in the northwest part of the Zemuhe fault and depressed in the southeast part of the Zemuhe fault zone, with a border somewhere between Puge and Ningnan Counties. Combined with microscopic groundwater, geodetic and seismic activity data, we infer that the anomalies in the Xichang area were the result of increasing tectonic activity in the Sichuan–Yunnan block. In addition, groundwater data may be used as a good indicator of tectonic activity. This case tells us that there is no direct relationship between an earthquake and these anomalies. In most cases, the vast majority of the anomalies, including microscopic and macroscopic anomalies, are caused by tectonic activity. That is, these anomalies could occur under the effects of tectonic activity, but they do not necessarily relate to the occurrence of earthquakes.</description><subject>Anomalies</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Earthquakes</subject><subject>Fault zones</subject><subject>Geophysics/Geodesy</subject><subject>Groundwater</subject><subject>Groundwater data</subject><subject>Groundwater levels</subject><subject>Hydrologic data</subject><subject>Rock deformation</subject><subject>Seismic activity</subject><subject>Surveying</subject><subject>Tectonics</subject><issn>0033-4553</issn><issn>1420-9136</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp1kE1PAjEURRujiYj-AHeTuK6-ftMlISgkJGwwLptSHjA4zEA7s-DfWzImrlzdzbn3JoeQZwavDMC8JQDgkgIzlCmrqb0hAyY5UMuEviUDACGoVErck4eUDpBBo-yATFYY2qYug6-qSzGvN13ATTGum6OvSkzFV9num64tFj7usJj62O7Pnf_GYhlCFyPWAdMjudv6KuHTbw7J5_t0NZnRxfJjPhkvqBfCtlRxu2aCSxHASmtNgLW1sGZSa42SS_AjL0MQHDVy4cNIey6V50EZUGGDYkhe-t1TbM4dptYdmi7W-dJxMEbkFyMzxXoqxCaliFt3iuXRx4tj4K6uXO_KZQXu6srZ3OF9J2W23mH8W_6_9AO-imri</recordid><startdate>20180701</startdate><enddate>20180701</enddate><creator>Shi, Zheming</creator><creator>Wang, Guangcai</creator><creator>Liu, Chenglong</creator><creator>Che, Yongtai</creator><general>Springer International Publishing</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>L7M</scope><scope>M2P</scope><scope>P5Z</scope><scope>P62</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><orcidid>https://orcid.org/0000-0002-9827-9008</orcidid></search><sort><creationdate>20180701</creationdate><title>Tectonically Induced Anomalies Without Large Earthquake Occurrences</title><author>Shi, Zheming ; 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Geophys</stitle><date>2018-07-01</date><risdate>2018</risdate><volume>175</volume><issue>7</issue><spage>2513</spage><epage>2526</epage><pages>2513-2526</pages><issn>0033-4553</issn><eissn>1420-9136</eissn><abstract>In this study, we documented a case involving large-scale macroscopic anomalies in the Xichang area, southwestern Sichuan Province, China, from May to June of 2002, after which no major earthquake occurred. During our field survey in 2002, we found that the timing of the high-frequency occurrence of groundwater anomalies was in good agreement with those of animal anomalies. Spatially, the groundwater and animal anomalies were distributed along the Anninghe–Zemuhe fault zone. Furthermore, the groundwater level was elevated in the northwest part of the Zemuhe fault and depressed in the southeast part of the Zemuhe fault zone, with a border somewhere between Puge and Ningnan Counties. 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subjects | Anomalies Earth and Environmental Science Earth Sciences Earthquakes Fault zones Geophysics/Geodesy Groundwater Groundwater data Groundwater levels Hydrologic data Rock deformation Seismic activity Surveying Tectonics |
title | Tectonically Induced Anomalies Without Large Earthquake Occurrences |
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