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 |