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Springwater Chemical Anomalies Prior To the Mw = 7.2 Van Earthquake (Turkey)

dc.authorscopusid 55400292100
dc.authorscopusid 35792853500
dc.authorscopusid 6602734183
dc.authorscopusid 57194965187
dc.authorscopusid 35739305500
dc.authorscopusid 7005731366
dc.contributor.author Inan, S.
dc.contributor.author Yakan, H.
dc.contributor.author Balderer, W.P.
dc.contributor.author Leuenberger-west, F.
dc.contributor.author Özvan, A.
dc.contributor.author Freund, F.T.
dc.date.accessioned 2025-05-10T16:59:48Z
dc.date.available 2025-05-10T16:59:48Z
dc.date.issued 2012
dc.department T.C. Van Yüzüncü Yıl Üniversitesi en_US
dc.department-temp Inan S., TÜBITAK Marmara Research Center, Earth and Marine Sciences Institute, Kocaeli, 41470, Gebze, Turkey; Yakan H., TÜBITAK Marmara Research Center, Earth and Marine Sciences Institute, Kocaeli, 41470, Gebze, Turkey; Balderer W.P., ETHZ, Engineering Geology, Sonneggstrasse 5 ETH Zentrum, CH 8092 Zürich, Swaziland; Leuenberger-west F., ETHZ, Engineering Geology, Sonneggstrasse 5 ETH Zentrum, CH 8092 Zürich, Swaziland; Özvan A., Van 100. Yil University, Department of Geology, 65040, Van, Turkey; Freund F.T., NASA Ames Research Center, Earth Science Division, CA 94035-1000, Code SGE, MS 242-4, Moffett Field, United States, Carl Sagan Center, SETI Institute, CA 94043, 189 Bernardo Ave. Mountain View, United States, Department of Physics, San Jose State University, San Jose, CA 95192-0106, United States en_US
dc.description.abstract We performed chemical analyses of commercially bottled spring water (EREK Spring water) emanating from a location less than 20 kilometer from the epicenter of the Mw = 7.2 Van Earthquake of October 23rd 2011. The available water samples cover the period from September 8th 2011 to January 11th 2012. The pre-earthquake anomaly is characterized by a slight but clear increase in Ca2+, Mg2+, K+ and Cl- contents and decrease in Na+ and SO42- contents compared to the background. Post-seismic samples show decreasing trends in Ca2+, Mg2+, K+ and Cl- and increasing trends in Na+ and SO42-. All ion concentrations reach stability approximately one month after the earthquake. These results indicate that spring water chemical anomalies may be monitored as potential geochemical pre-earthquake indicators. © 2012, GEOCHEMICAL SOCIETY OF JAPAN. All rights reserved. en_US
dc.identifier.doi 10.2343/geochemj.1.0159
dc.identifier.issn 0016-7002
dc.identifier.issue 1 en_US
dc.identifier.scopus 2-s2.0-85024451443
dc.identifier.scopusquality Q3
dc.identifier.uri https://doi.org/10.2343/geochemj.1.0159
dc.identifier.uri https://hdl.handle.net/20.500.14720/4772
dc.identifier.volume 46 en_US
dc.identifier.wosquality Q4
dc.language.iso en en_US
dc.relation.ispartof Geochemical Journal en_US
dc.relation.publicationcategory Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı en_US
dc.rights info:eu-repo/semantics/openAccess en_US
dc.subject Earthquake Precursors en_US
dc.subject Geochemical Anomalies en_US
dc.subject Spring Water en_US
dc.subject Turkey en_US
dc.subject Van en_US
dc.title Springwater Chemical Anomalies Prior To the Mw = 7.2 Van Earthquake (Turkey) en_US
dc.type Article en_US

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